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Basics Of Global Monsoon Time Scales China Type Climate Region & China Type Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: China type Climate – Warm Temperate Eastern Margin Climate. This type of climate is found on the eastern margin of continent in warm temperate latitudes, just outside the tropics & comparatively has more rainfall than the Mediterranean climate in the same latitudes, coming mainly in summers. Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and China type Climate Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and China type Climate Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales China Type Climate Region & China Type Climate Time Scale. Rep Opinion 2017;9(11s):1-3]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 1. doi:10.7537/marsroj0911s17.01.

Key Words: China type Climate Region, China type Climate Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale

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Basics Of Global Monsoon Time Scales Cold Climate Region & Cold Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: These climates have an average temperature above 10 °C in their warmest months, and a coldest month average below −3 °C. These usually occur in the interiors of continents, or on their east coasts, north of 40° North latitude. In the Southern Hemisphere, this climate is extremely rare due to the smaller land masses in the middle latitudes and the almost complete absence of land south of 40° South latitude, existing only in some highland locations in New Zealand that have heavy winter snows. Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Cold Climate Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Cold Climate Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Cold Climate Region & Cold Climate Time Scale. Rep Opinion 2017;9(11s):4-6]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 2. doi:10.7537/marsroj0911s17.02.

Key Words: Cold Climate Region, Cold Climate Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale

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Basics Of Global Monsoon Time Scales Cold Desert Climate Region & Cold Desert Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: Cold desert climates (BWk) usually feature hot (or warm in a few instances), dry summers, though summers typically are not quite as hot as summers in hot desert climates. Unlike hot desert climates, cold desert climates tend to feature cold winters dry winters. Snow tends to be rare in regions with this climate. The Gobi Desert in Mongolia is a classic example of this. Though hot in summer, it shares the very cold winters of the rest of Central Asia. Cold desert climates are typically found at higher altitudes than hot desert climates, and are usually drier than hot desert climates. Cold desert climates are typically located in temperate zones, usually in the rain shadow of high mountains, which restrict precipitation from the westerly winds. An example of this is the Patagonian Desert in Argentina bounded by the Andes to its west. In the case of Central Asia, mountains restrict precipitation from the monsoon. The Kyzyl Kum, Taklamakan and Katpana Desert deserts of Central Asia and the drier portions of the Great Basin Desert of the western United States are other major examples of BWK climates. The Ladakh region, and Lehacity in the Great Himalayas in India also has a cold desert climate. This is also found in Europe, primarily in Barde Reales near Tudela, Navarre and high altitude parts of the Tabernas Desert in Almería, Spain and the Karagiye Depression in Aktau, Kazakhstan. Arctic and Antarctic regions also receive very little precipitation during the year, owing to the exceptionally cold dry air, however, both of them are generally classified as having polar climates because they have average summer temperatures below 10 °C (50 °F). Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Cold Desert Climate Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Cold Desert Climate Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Cold Desert Climate Region & Cold Desert Climate Time Scale. Rep Opinion 2017;9(11s):7-9]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 3. doi:10.7537/marsroj0911s17.03.

Key Words: Cold Desert Climate Region, Cold Desert Climate Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale

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Basics Of Global Monsoon Time Scales Continental Climate Region & Continental Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Continental Climate Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Continental Climate Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Continental Climate Region & Continental Climate Time Scale. Rep Opinion 2017;9(11s):10-12]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 4. doi:10.7537/marsroj0911s17.04.

Key Words: Continental Climate Region, Continental Climate Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale

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Basics Of Global Monsoon Time Scales Continental Warm Summer Climate & Continental Summer Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: A humid continental climate (Köppen prefix D and a third letter of a or b) is a climatic region defined by Russian-German climatologist Wladimir Köppen in 1900, which is typified by large seasonal temperature differences, wit warm to hot (and often humid) summers and cold (sometimes severely cold) winters. Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Continental Summer Climate Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Continental Warm Summer Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Continental Warm Summer Climate & Continental Summer Climate Time Scale. Rep Opinion 2017;9(11s):13-15]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 5. doi:10.7537/marsroj0911s17.05.

Key Words: Continental Warm Summer Climate, Continental Warm Summer Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale.

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Basics Of Global Monsoon Time Scales Desert Climate Region & Desert Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: The Desert climate BWh and BWk, sometimes also BWn), also known as an arid climate, is a climate that does not meet the criteria to be classified as a polar climate, and in which precipitation is too low to sustain any vegetation at all, or at most a very scanty shrub. An area that features this climate usually experiences from 25 to 200 mm (7.87 inches) per year of precipitation and in some years may experience no precipitation at all. There are usually two or three variations of a desert climate: a hot desert climate (BWh), a cold desert climate (BWk) and, sometimes, a mild desert climate (BWh/BWn). To determine whether a location has an arid climate, the precipitation threshold is determined. The precipitation threshold (in millimetres) involves first multiplying the average annual temperature in °C by 20, then adding 280 if 70% or more of the total precipitation is in the high-sun half of the year (April through September in the Northern Hemosphear or October through March in the Southern), or 140 if 30–70% of the total precipitation is received during the applicable period, or 0 if less than 30% of the total precipitation is so received. If the area's annual precipitation is less than half the threshold, it is classified as a BW (desert climate) Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Desert Climate Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Desert Climate Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Desert Climate Region & Desert Climate Time Scale. Rep Opinion 2017;9(11s):16-18]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 6. doi:10.7537/marsroj0911s17.06.

Key Words: Desert Climate Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale.

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Basics Of Global Monsoon Time Scales Dry Arid Climate Region & Dry Arid Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: The word Arid means Dry. The two colors on the map represent warm and cold Arid Climates. If land has an Arid Climate it is usually a desert. Most deserts are found along the 30 degree latitude line (north and south of the equato). Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Dry Arid Climate Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Dry Arid Climate Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Dry Arid Climate Region & Dry Arid Climate Time Scale. Rep Opinion 2017;9(11s):19-21]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 7. doi:10.7537/marsroj0911s17.07.

Key Words: Dry Arid Climate Region, Dry Arid Climate Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale.

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Basics Of Global Monsoon Time Scales Dry Climate Region & Dry Climate Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: The word arid means Dry. The two colors on the map represent warm and cold Arid Climates. If land has an Arid Climate it is usually a desert. Most deserts are found along the 30 degree latitude line (north and south of the equator). Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Dry Climate Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Dry Climate Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Dry Climate Region & Dry Climate Climate Time Scale. Rep Opinion 2017;9(11s):22-24]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 8. doi:10.7537/marsroj0911s17.08.

Key Words: Dry Climate Region, Dry Climate Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale

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Equatorial Climate Region & Equatorial Climate Time Scale

Gangadhara Rao Irlapati

H.NO.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad, India-500055

Email: scientistgangadhar@gmail.com

Abstract: Many regions close to the equator experience an Equatorial Climate. These regions include, the Amazon Basin (South America), the Congo Basin (Africa), Malaysia, Indonesia and some areas in northern Australia. Regions with this climate experience high temperatures all year round. The average monthly temperatures are about 26 – 28 degrees Celsius. The annual temperature range (the difference between the average temperature of the hottest and coldest months) is very small. The annual temperature range may be as low as 3 degrees Celsius. The diurnal or daily temperature range (the difference between the highest temperature in the day and the lowest temperature at night) is usually greater. Humidity is usually very high. Another major characteristic of this climate is the high rainfall. These regions usually experience 2000 mm of rainfall or more in a year. Rainfall is high for most of the year. Many equatorial regions are affected by the ITCZ. As the ITCZ passes over these areas it brings heavy rainfall and thunderstorms. In some areas, the ITCZ causes two periods of very heavy rainfall every year. One occurs when the ITCZ crosses these areas on its way north and another occurs when it crosses these areas again on its way south. The climograph below shows the rainfall and temperature pattern of an area which experiences an equatorial climate.

[Gangadhara Rao Irlapati. Equatorial Climate Region & Equatorial Climate Time Scale. Rep Opinion 2017;9(11s):25-28]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 9. doi:10.7537/marsroj0911s17.09.

Key Words: Equatorial climate, Global Monsoon Time Scale, Indian Monsoon Time Scale

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Basics Of Global Monsoon Time Scales Highland Climate Articles Region & Highland Climate Articles Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: Highland climate is the climate of 'high' 'land'. So, this climate is found in high mountain areas. It is found on single mountains such as Mount Kilimanjaro and also large areas of high elevation such as the Plateau of Tibet. any studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Highland Climate Articles Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Highland Climate Articles Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Highland Climate Articles Region & Highland Climate Articles Time Scale. Rep Opinion 2017;9(11s):29-31]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 10. doi:10.7537/marsroj0911s17.10.

Key Words: Highland Climate Articles Region, Highland Climate Articles Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale.

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Basics Of Global Monsoon Time Scales Hot Desert Climate Region & Hot Desert Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: Hot desert climates (BWh) are typically found under the subtropical ridge where there is largely unbroken sunshine for the whole year due to the stable descending air and high pressure aloft. These areas are located between 30 degrees south and 30 degrees north latitude, under the subtropical latitudes called the horse latitudes. Hot desert climates are generally hot, sunny and dry year-round. Hot desert climates also reach similar latitudes in the Middle East, North Africa, and coastal south eastern areas of Spain. Part of the Canary Islands. (specially most of Fuerteventura and Lanzarote have hot desert climates^. Hot desert climates usually feature hot, sometimes exceptionally hot, periods of the year. The world absolute heat records, over 50 °C (122 °F), are generally in the hot deserts, where the heat potential is the highest on the planet. Some desert locations consistently experience very high temperatures all year long, even during wintertime. Hot desert climates can be found in the deserts of North Africa such as the wide Sahara Desert, the Libyan Desert or the Nubian Desert deserts of the Horn of Africa such as the Danakil Deser or the Grand Bara Desert deserts of Southern Africa such as the Namib Desert or the Kalahari Desert deserts of the Middle East such as the Arabian Desert, the Syrian Desert or the Lut Desert, deserts of South Asia such as Dasht-e Kavir, Dasht-e Loot, or the Thar Desert, deserts of the United States and Mexico such as the Mojave Desert, the Sonoran Desert or the deserts of Australia such as the Simpson Desert or the Great Victoria Desert and many other regions. Only one region in Europe has a hot desert climate, the Almería and a small area in the southwest of Murcia and Alicante, Spain. Hot deserts are lands of extremes: most of them are the hottest, the driest and the sunniest places on Earth because of nearly constant high pressure; the nearly permanent removal of low pressure systems, dynamic fronts and atmospheric disturbances; sinking air motion; dry atmosphere near the surface and aloft; the exacerbated exposure to the sun where solar angles are always high. Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Hot Desert ClimateTime Scalewhich can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Hot Desert Climate Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Hot Desert Climate Region & Hot Desert Climate Time Scale. Rep Opinion 2017;9(11s):32-34]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 11. doi:10.7537/marsroj0911s17.11.

Key Words: Hot Desert Climate Region, Hot Desert Climate Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale

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Basics Of Global Monsoon Time Scales Hot Se3mi-Arid Climate Region & Hot Semi-Arid Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: Hot semi-arid climates (type "BSh") tend to be located in the 20s and 30s latitudes, typically in close proximity to regions with a tropical savanna climate or a humid subtropical climate. These climates tend to have hot, sometimes extremely hot, summers and warm to cool winters, with some to minimal precipitation. Hot semi-arid climates are most commonly found around the fringes of subtropical deserts. Hot semi-arid climates are most commonly found in Africa, Australia and South Asia. In Australia, a large portion of the Outback surrounding the central desert regions lies within the hot semi-arid climate regime. In South Asia, both India and sections of Pakistan experiences the seasonal effects of monsoons and feature short but well-defined wet seasons, but is not sufficiently wet overall to qualify as a tropical savanna climate. Hot semi-arid climates can also be found in North America, primarily in Mexico, areas of Texas near Mexico and sections of Southern California. It can also be found in sections of South America such as the sertão and on the poleward side of the arid deserts where they typically feature a Mediterranean precipitation pattern, with generally rainless summers and wetter winters Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Hot Semi Arid Climate Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Hot Semi Arid Climate Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Hot Se3mi-Arid Climate Region & Hot Semi-Arid Climate Time Scale. Rep Opinion 2017;9(11s):35-37]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 12. doi:10.7537/marsroj0911s17.12.

Key Words: Hot Semi Arid Climate Region, Hot Semi Arid Climate Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale.

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Basics Of Global Monsoon Time Scales Humid Subtropical Climate Region & Humid Subtropical Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: A humid subtropical climate is a zone of climate characterised by hot and humid summers where tropical air masses dominate, and mild winters. These climates normally lie on the southeast side of all continents, genrally between latitudes 25° and 35° and are adjacent to tropical climates to the south. Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Humid Subtropical Climate Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Humid Subtropical Climate Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Humid Subtropical Climate Region & Humid Subtropical Climate Time Scale. Rep Opinion 2017;9(11s):38-40]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 13. doi:10.7537/marsroj0911s17.13.

Key Words: Humid Subtropical Climate Region, Humid Subtropical Climate Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale

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Basics Of Global Monsoon Time Scales Ice Cap Climate Region & Ice Cape Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: An ice cap climate is a polar climate where the temperature never exceeds 0 °C (32 °F). The climatecovers areas in or near the polar regions, such as Antarctica and Greenland, as well as the highest mountaintops. Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Ice Cape Climate Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Ice Cape Climate Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Ice Cap Climate Region & Ice Cape Climate Time Scale. Rep Opinion 2017;9(11s):41-43]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 14. doi:10.7537/marsroj0911s17.14.

Key Words: Ice Cape Climate Region, Ice Cape Climate Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale.

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Basics Of Global Monsoon Time Scales Mid-Latitude Climate Region & Mid-Latitude Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: The middle latitudes (mid-latitudes, sometimes midlatitudes) are between 23°26'22" North and 66°33'39" North, and between 23°26'22" South and 66°33'39" South latitude, or, the Earth's temperate zones between the ropics and the Arctic and Antarctic polar regions. Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Mid-Lattitude Climate Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Mid-Lattitude Climate Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Mid-Latitude Climate Region & Mid-Latitude Climate Time Scale. Rep Opinion 2017;9(11s):44-46]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 15. doi:10.7537/marsroj0911s17.15.

Key Words: Mid-Lattitude Climate Regoin, Mid-Lattitude Climate Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale.

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Basics Of Global Monsoon Time Scales Mild Deseryt Climate Region & Mild Desert Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: Mild desert climates (BWh or BWn) are usually found along the west coasts of continents at tropical or near tropical locations, or at high altitudes in areas that would otherwise feature hot desert climates. In South America, this climate is found adjacent to the Pacific Ocean in sections of the Atacama Desert, especially along the central and southern coast of Peru, Lima, its capital, has a mild desert climate that makes it one of the driest capital cities in the world. In North America, this type of climate can be found along the Pacific coast of the Baja California Peninsula. In Africa, this climate is found along sections of coastal Namibia Swakopmund. On the Arabia Peninsula, this type of climate is found in sections of Yemen. Mild desert climates are characterised by more moderate temperatures than encountered elsewhere at comparable latitudes (usually due to the nearby presence of cold ocean currents) and, in the case of coastal mild deserts, frequent fog and low clouds, despite the fact that these places can rank among the driest on Earth in terms of actual precipitation received. Temperatures are mild throughout the year, usually not subject to any of the temperature extremes typically found in desert climates. Some publications do not have a "mild desert" category; in these documents mild desert climates are sorted into either the hot desert or cold desert classification. Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Mild Desert Climate Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Mild Desert Climate Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Mild Deseryt Climate Region & Mild Desert Climate Time Scale. Rep Opinion 2017;9(11s):47-49]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 16. doi:10.7537/marsroj0911s17.16.

Key Words: Mild Desert Climate Region, Mild Desert Climate Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale

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Basics Of Global Monsoon Time Scales Moist Midlatitudes Cold Winter Climate & Moist Midlatitude Cold Winter Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: Moist continental mid-latitude climates have warm to cool summers and cold winters. The location of these climates is pole ward of the C climates. The average temperature of the warmest month is greater than 10° Celsius, while the coldest month is less than -3° Celsius. Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Moist Midlatitude Climate Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Moist Midlatitude Climate Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Moist Midlatitudes Cold Winter Climate & Moist Midlatitude Cold Winter Climate Time Scale. Rep Opinion 2017;9(11s):50-52]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 17. doi:10.7537/marsroj0911s17.17.

Key Words: Moist Midlatitude Climate Region, Moist Midlatitude Climate Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale

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Basics Of Global Monsoon Time Scales Moist Midlatitudes Mild Winter Climate & Moist Midlatitude Mild Winter Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: The humid subtropical climate (Cfa) has hot muggy summers and mainly thunderstorms. Winters are mild and precipitation during this season comes frommid-latitude cyclones.... Cfb, marine, climates are found on the western coasts of continents. They have a humid climate with short dry summer. Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Moist Midlatitude Mild Winter Climate Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Moist Midlatitude Mild Winter Climate Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Moist Midlatitudes Mild Winter Climate & Moist Midlatitude Mild Winter Climate Time Scale. Rep Opinion 2017;9(11s):53-55]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 18. doi:10.7537/marsroj0911s17.18.

Key Words: Moist Midlatitude Mild Winter Climate Region, Moist Midlatitude Mild Winter Climate Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale

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Basics Of Global Monsoon Time Scales Mountains Tundra Climate Region & Mountains Tundra Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Mountains Tundra Climate Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Mountains Tundra Climate Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Mountains Tundra Climate Region & Mountains Tundra Climate Time Scale. Rep Opinion 2017;9(11s):56-58]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 19. doi:10.7537/marsroj0911s17.19.

Key Words: Mountains Tundra Climate Region, Mountains Tundra Climate Time Scale., Indian Monsoon Time Scale, Global Monsoon Time Scale.

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Basics Of Global Monsoon Time Scales Oceanic Climate Region & Oceanic Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: An Oceanic Climate (also known as marine, west coast and maritime) is the Köppen classification of the climate typical of west coasts in higher middle latitudes of continents, and generally features cool summers (relative to their latitude) and cool but not cold winters, with a relatively narrow annual temperature range and few extremes of temperature, with the exception for transitional areas to continental, subarctic and highland climates. Oceanic climates are defined as having a monthly mean temperature below 22 °C (72 °F) in the warmest month, and above 0°C (32°F) in the coldest month. It typically lacks a dry season, as precipitation is more evenly dispersed throughout the year. It is the predominant climate type across much of Western Europe, the Pacific Northwest region of the United States and Canada, portions of central Mexico, southwestern South America, southeastern Australia including Tasmania, New Zealand as well as isolated locations elsewhere. Oceanic climates generally have cool summers and cool (but not cold) winters. They are characterised by a narrower annual range of temperatures than are encountered in other places at a comparable latitude, and generally do not have the extremely dry summers of Mediterranean climates or the hot summers of humid subtropical Oceanic climates are most dominant in Europe, where they spread much farther inland than in other continents. Oceanic climates can have much storm activity as they are located in the belt of the stormy westerlies. Many oceanic climates have frequent cloudy or overcast conditions due to the near constant storms and lows tracking over or near them. The annual range of temperatures is smaller than typical climates at these latitudes due to the constant stable marine air masses that pass through oceanic climates, which lack both very warm and very cool fronts. Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Oceanic Climate Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Oceanic Climate Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Oceanic Climate Region & Oceanic Climate Time Scale. Rep Opinion 2017;9(11s):59-61]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 20. doi:10.7537/marsroj0911s17.20.

Key Words: Oceanic Climate Region, Oceanic Climate Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale.

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Basics Of Global Monsoon Time Scales Polar Climate Region & Polar Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: The polar climate regions are characterized by a lack of warm summers. Every month in a polar climatehas an average temperature of less than 10 °C (50 °F). Regions with polar climate cover more than 20% of the Earth. The sun shines for long hours in the summer, and for many fewer hours in the winter. Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Polar Climate Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Polar Climate Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Polar Climate Region & Polar Climate Time Scale. Rep Opinion 2017;9(11s):62-64]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 21. doi:10.7537/marsroj0911s17.21.

Key Words: Polar Climate Region, Polar Climate Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale.

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Basics Of Global Monsoon Time Scales Polar Tundra Climate Region & Polar Tundra Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: Regions with polar climate cover more than 20% of the Earth. The sun shines for long hours in the summer, and for many fewer hours in the winter. Apolar limate results in treeless tundra, glaciers, or a permanent or semi-permanent layer of ice. It has cool summers and very cold winters. Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Polar Tundra Climate Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Polar Tundra Climate Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Polar Tundra Climate Region & Polar Tundra Climate Time Scale. Rep Opinion 2017;9(11s):65-57]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 22. doi:10.7537/marsroj0911s17.22.

Key Words: Polar Tundra Climate Region., Polar Tundra Climate Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale.

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Basics Of Global Monsoon Time Scales Rainforest Climate Region & Rainforest Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: Rainforest Climate. In an average year in a tropical rain Forest, the Climate is very humid because of all the rainfall, which amounts to about 250 cm per year. The Rain Forest has lots of rain because it is very hot and wet. This Climate is found near the equator. A Tropical Rainforest Climate, also known as an Equatorial Climate, is a tropical climate usually (but not always) found along the equator. Regions with this climate typically feature tropical rainforests, and it is designated Af by the Köppen climate classification. Tropical rainforests have a type of tropical climate in which there is no dry season—all months have an average precipitation value of at least 60 mm (2.4 in). Tropical rainforests have no summer or winter; it is typically hot and wet throughout the year and rainfall is both heavy and frequent. One day in an equatorial climate can be very similar to the next, while the change in temperature between day and night may be larger than the average change in temperature along the year Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Rainforest Climate Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Rainforest Climate Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Rainforest Climate Region & Rainforest Climate Time Scale. Rep Opinion 2017;9(11s):68-70]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 23. doi:10.7537/marsroj0911s17.23.

Key Words: Rainforest Climate Regoin, Rainforest Climate Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale

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Basics Of Global Monsoon Time Scales Semi Arid Climate Region & Semi Arid Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: A semi-arid climate or steppe climate is the climate of a region that receives precipitation below potential evapotranspiration, but not extremely. There are different kinds of semi-arid climates, depending on such variables as temperature, and they give rise to different classes of ecology. A more precise definition is given by the Köppen climate classification, which treats steppe climates (BSk and BSh) as intermediates between desert climates, (BW) and humid climates in ecological characteristics and agricultural potential. Semi-arid climates tend to support short or scrubby vegetation, with semi-arid areas usually dominated by either grasses or shrubs. To determine if a location has a semi-arid climate, the precipitation threshold must first be determined. Finding the precipitation threshold (in millimeters) involves first multiplying the average annual temperature in °C by 20, then adding 280 if 70% or more of the total precipitation is in the high-sun half of the year (April through September in the Northern temperate zone, or October through March in the Southern), or 140 if 30%–70% of the total precipitation is received during the applicable period, or 0 if less than 30% of the total precipitation is so received. If the area's annual precipitation is less than the threshold but more than half the threshold, it is classified as a BS (steppe climate). Furthermore, to delineate "hot semi-arid climates" from "cold semi-arid climates", there are three widely used isotherms, Either a mean annual temperature of 18°C, or a mean temperature of 0°C or −3°C in the coldest month, so that a location with a "BS" type climate with the appropriate temperature above whichever isotherm is being used is classified as "hot semi-arid" (BSh), and a location with the appropriate temperature below the given isotherm is classified as "cold semi-arid" (BSk) Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Semi Arid Climate Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Semi Arid Climate Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Semi Arid Climate Region & Semi Arid Climate Time Scale. Rep Opinion 2017;9(11s):71-73]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 24. doi:10.7537/marsroj0911s17.24.

Key Words: Semi Arid Climate Region, Semi Arid Climate Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale

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Basics Of Global Monsoon Time Scales Snow Forest Climate Region & Snoe Forest Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: It is distinguished from the dry Climates by a function of annual temperature and precipitation (see formulas under steppe Climate). The outstanding feature of these Climates is the cold winters with at least a month of snow-covered ground. These are the coldest of the tree Climate Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Snowforest Climate Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Snowforest Climate Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Snow Forest Climate Region & Snoe Forest Climate Time Scale. Rep Opinion 2017;9(11s):74-76]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 25. doi:10.7537/marsroj0911s17.25.

Key Words: Snowforest Climate Region, Snowforest Climate Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale.

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Basics Of Global Monsoon Time Scales St Lawrence Type Climate Region & St Lawrence Type Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: The climate in St. Lawrence is warm and temperate. St. Lawrence is a city with a significant rainfall. Even in the driest month there is a lot of rain. According to Köppen and Geiger, this climate is classified as Cfb. The average annual temperature in St. Lawrence is 11.7 °C. About 857 mm of precipitation falls annually. Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and ST Lawrence Type TIME SCALE which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and ST Lawrence Type TIME SCALE.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales St Lawrence Type Climate Region & St Lawrence Type Climate Time Scale. Rep Opinion 2017;9(11s):77-79]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 26. doi:10.7537/marsroj0911s17.26.

Key Words: ST Lawrence Type Region, ST Lawrence Type TIME SCALE, Indian Monsoon Time Scale, Global Monsoon Time Scale.

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Basics Of Global Monsoon Time Scales Steppe Type Climate Region & Steppe Type Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: A steppe is a dry, grassy plain. Steppes occur intemperate climates, which lie between the tropics and polar regions. Temperate regions have distinct seasonal temperature changes, with cold wintes and warm summers. Steppes are semi-arid, meaning they receive 25 to 50 centimeters (10-20 inches) of rain each year. Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Steppe Type Climate Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Steppe Type Climate Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Steppe Type Climate Region & Steppe Type Climate Time Scale. Rep Opinion 2017;9(11s):80-82]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 27. doi:10.7537/marsroj0911s17.27.

Key Words: Steppe Type Climate Region, Steppe Type Climate Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale

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Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: An Oceanic Climate (also known as marine, west coast and maritime) is the Köppen classification of the climate typical of west coasts in higher middle latitudes of continents, and generally features cool summers (relative to their latitude) and cool but not cold winters, with a relatively narrow annual temperature. Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Sub Tropical Highland Climate Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Sub Tropical Highland Climate Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Sub Tropical Highland Climate Region & Sub Tropical Highland Climate Time Scale. Rep Opinion 2017;9(11s):83-85]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 28. doi:10.7537/marsroj0911s17.28.

Key Words: Sub Tropical Highland Climate Region, Sub Tropical Highland Climate Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale

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Basics Of Global Monsoon Time Scales Taiga Type Climate Region & Taiga Type Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: The lowest reliably recorded temperatures in the Northern Hemisphere were recorded in the Taiga of northeastern Russia. The Taiga or boreal forest has a subarctic Climate with very large temperature range between seasons, but the long and cold winter is the dominant feature. Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Taiga Type Climate Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Taiga Type Climate Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Taiga Type Climate Region & Taiga Type Climate Time Scale. Rep Opinion 2017;9(11s):86-88]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 29. doi:10.7537/marsroj0911s17.29.

Key Words: Taiga Type Climate Region, Taiga Type Climate Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale

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Basics Of Global Monsoon Time Scales Temperate Climate Region & Temperate Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: Temperate climates are those without extremes of temperature and precipitation (rain and snow). The changes between summer and winter are generally invigorating without being frustratingly extreme. There are two types of temperate climate: maritime and continental. Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Temperate Climate Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Temperate Climate Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Temperate Climate Region & Temperate Climate Time Scale. Rep Opinion 2017;9(11s):89-91]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 30. doi:10.7537/marsroj0911s17.30.

Key Words: Temperate Climate Region, Temperate Climate Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale

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Basics Of Global Monsoon Time Scales Tropical Monsoon Climate Region & Tropical Monsoon Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: The tropical monsoon climate experiences abundant rainfall like that of the tropical rain forest climate, but it is concentrated in the high-sun season. Being located near the equator, the tropical monsoon climate experiences warm temperatures throughout the year. The monsoon climate is found along the coastal regions of southwest India, sri lanka, bangladesh, Southwestern Africa, French Guina and northeast and southeastern Brazil etc. The major controlling factor over the monsoon climate is its relationship to the monsoon circulation. Recall that the monsoon is a seasonal change in wind direction. The "classic" monsoon circulation of Asia exhibits an onshore flow of air (air moving from ocean towards land) during the summer or high-sun season, and offshore air flow (air moving from land toward water) during the winter or low-sun season. The change in direction is due to the difference in the way water and land heat. Changing pressure patterns that affect the seasonality of precipitation also occur in Africa. During the high-sun season, the ITCZ induces rain while the subtropical high creates dry conditions. The monsoon climate of Africa, and South America for that matter, are typically located along tradewind coasts. Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Tropical Monsoon Climate Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Tropical Monsoon Climate Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Tropical Monsoon Climate Region & Tropical Monsoon Climate Time Scale. Rep Opinion 2017;9(11s):92-94]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 31. doi:10.7537/marsroj0911s17.31.

Key Words: Tropical Monsoon Climate Region, Tropical Monsoon Climate Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale.

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Basics Of Global Monsoon Time Scales Tropical And Subtropical Desert Climate & Tropical And Subtropical Desert Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: Tropical and subtropical desert climate, major climate type of the Köppen classification dominated in all months by the subtropical anticyclone (orsubtropical high), with its descending air, elevated inversins, and clear skies. Such an atmospheric environment inhibits precipitation. Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Tropical and Subtropical Climate Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Tropical and Subtropical Climate Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Tropical And Subtropical Desert Climate & Tropical And Subtropical Desert Climate Time Scale. Rep Opinion 2017;9(11s):95-97]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 32. doi:10.7537/marsroj0911s17.32.

Key Words: Tropical and Subtropical Climate Region, Tropical and Subtropical Climate Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale

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Basics Of Global Monsoon Time Scales Tropical Savanna Climate Region & Tropical Savanna Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: Tropical Savanna Climate or Tropical Wet And Dry Climate is a type of climate that corresponds to the Köppen climate classification categories "Aw" and "As". Tropical savanna climates have monthly mean temperatures above 18 °C (64 °F) in every month of the year and typically a pronounced dry season, with the driest month having precipitation less than 60 mm and also less than 100 – [total annual precipitation {mm}/25] of precipitation.^[1]:200–1 This latter fact is in direct contrast to a tropical monsoon climate, whose driest month sees less than 60 mm of precipitation but has more than 100 – [total annual precipitation {mm}/25] of precipitation. In essence, a tropical savanna climate tends to either see less rainfall than a tropical monsoon climate or have more pronounced dry Seasons. There are generally four types of tropical savanna climate. Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Tropical Savanna Climate Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Tropical Savanna Climate Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Tropical Savanna Climate Region & Tropical Savanna Climate Time Scale. Rep Opinion 2017;9(11s):98-100]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 33. doi:10.7537/marsroj0911s17.33.

Key Words: Tropical Monsoon Climate Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale

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Basics Of Global Monsoon Time Scales Tundra Climate Region & Tundra Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: Tundras are among Earth's coldest, harshest biomes.Tundra ecosystems are treeless regions found in the Arctic and on the tops of mountains, where the climate is cold and windy and rainfall is scant. Tundralands are snow-covered for much of the year, until summer brings a burst of wildflowers Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Tundra Climate Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Tundra Climate Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Tundra Climate Region & Tundra Climate Time Scale. Rep Opinion 2017;9(11s):101-103]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 34. doi:10.7537/marsroj0911s17.34.

Key Words: Tundra Climate Region, Tundra Climate Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale.

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Basics Of Global Monsoon Time Scales Tundra Climate Region & Tundra Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: Tundras are among Earth's coldest, harshest biomes. Tundra ecosystems are treeless regions found in the Arctic and on the tops of mountains, where the climate is cold and windy and rainfall is scant. Tundra lands are snow-covered for much of the year, until summer brings a burst of wildflowers Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Tundra Climate Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Tundra Climate Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Tundra Climate Region & Tundra Climate Time Scale. Rep Opinion 2017;9(11s):104-106]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 35. doi:10.7537/marsroj0911s17.35.

Key Words: Tundra Climate Region, Tundra Climate Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale.

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Basics Of Global Monsoon Time Scales Western European Type Climate Region & Western European Type Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: The Climate of Western Europe is strongly conditioned by the Gulf Stream, which keeps mild air (for the latitude) over Northwestern Europe in the winter months, especially in Ireland, the UK and coastal Noray. Parts of the central European plains have a hybrid oceanic/continental Climate. Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Western European Climate Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Western European Climate Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Western European Type Climate Region & Western European Type Climate Time Scale. Rep Opinion 2017;9(11s):107-109]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 36. doi:10.7537/marsroj0911s17.36.

Key Words: Western European Climate Region, Western European Climate Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale.

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Basics Of Global Monsoon Time Scales Cold Mid Latitude West European Climate Region & Cold Mid Latitude West European Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: Regions of this type are found on the western margins of the continents in the perma­nent zone of westerlies. It includes Western Europe from Northern Norway to British Isles, North-West United States, and Southern Chile in South America and Tasmania Island of New Zealand in Australia. This region is under the influence of westerly winds throughout the year. The winters are warmer and annual rainfall is higher than in cool East Margin Region. Rainfall is of cyclonic origin and occurs throughout the year with a maximum in winter. The mean annual range of temperature is below 15°C in European and North American Regions. Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Cold Mid Latitude West European Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Cold Mid Latitude West European Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Cold Mid Latitude West European Climate Region & Cold Mid Latitude West European Climate Time Scale. Rep Opinion 2017;9(11s):110-112]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 37. doi:10.7537/marsroj0911s17.37.

Key Words: Cold Mid Latitude West European Region, Cold Mid Latitude West European Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale

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Basics Of Global Monsoon Time Scales East Margin Climate Region & East Margin Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: It lies on the eastern margins of the continents in subtropical belt between 20° and 48° latitude in both hemispheres. The main characteris­tics of this region are summers are warm and moist and winters are cold, and during summer, trade winds blow from adjoining ocean and moderate rainfall occurs which decreases towards the equator and in winter, westerly winds blow from the interior towards the oceans. These land winds do not give rainfall and so winters are dry. Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and East Margin Climate Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and East Margin Climate Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales East Margin Climate Region & East Margin Climate Time Scale. Rep Opinion 2017;9(11s):113-115]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 38. doi:10.7537/marsroj0911s17.38.

Key Words: East Margin Climate Region, East Margin Climate Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale

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Basics Of Global Monsoon Time Scales Eastern Margins Climate Region & Eastern Margins Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: This region lies poleward of the Warm East Margin Region. The region has warm wet summer and cold dry winters. North Eastern United States and adjoining parts of Canada, North China, Manchuria, Korea, and Northern Japan are the main ar­eas included in this Region. Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Eastern Margins Climate Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Eastern Margins Climate Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Eastern Margins Climate Region & Eastern Margins Climate Time Scale. Rep Opinion 2017;9(11s):116-118]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 39. doi:10.7537/marsroj0911s17.39.

Key Words: Eastern Margins Climate Region, Eastern Margins Climate Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale

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Basics Of Global Monsoon Time Scales Equatorial Region & Equatorial Region Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: The equatorial belt extends roughly between 5°N and 5°S of the Equator. It has uniformly hot and wet climatic conditions throughout the year. The annual range of temperature is low, and seasonal contrasts are at a minimum. The combination of high temperature and high humidity makes the climate unfavourable for sustained human effort, but very favourable for the growth of vegetation. Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Equatorial Climate Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Equatorial Climate Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Equatorial Region & Equatorial Region Climate Time Scale. Rep Opinion 2017;9(11s):81-82]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 40. doi:10.7537/marsroj0911s17.40.

Key Words: Equatorial Climate Region, Equatorial Climate Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale

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Basics Of Global Monsoon Time Scales Mediterranian Climate Region & Mediterranian Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: This region lies poleward of the tropical deserts on the western margin of the conti­nents, roughly between 30° and 40° N and S lati­tudes. The summers are hot and dry while winters are mild and rainy. summer, trade winds blow from land to sea giving practically no rain. In winters, this region comes under the influence of moist wester­lies blowing on-shore and bringing cyclonic rain. Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Mediterranian Climate Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Mediterranian Climate Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Mediterranian Climate Region & Mediterranian Climate Time Scale. Rep Opinion 2017;9(11s):122-124]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 41. doi:10.7537/marsroj0911s17.41.

Key Words: Mediterranian Climate Region, Mediterranian Climate Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale.

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Basics Of Global Monsoon Time Scales Mid Latitudegrassland Climate Region & Mid Latitude Grassland Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: This region lies in the interior of the continents and therefore receives low rainfall. The annual range of temperature is high between warm summer and cold winter. Rainfall occurs as a result of convectional ascent of air during summer. Owing to low rainfall and cold winter, trees are generally absent. Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Mid Latitude Grassland Climate Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Mid Latitude Grassland Climate Time Scale

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Mid Latitudegrassland Climate Region & Mid Latitude Grassland Climate Time Scale. Rep Opinion 2017;9(11s):125-127]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 42. doi:10.7537/marsroj0911s17.42.

Key Words: Mid Latitude Grassland Climate Region, Mid Latitude Grassland Climate Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale.

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Basics Of Global Monsoon Time Scales Mid Latitude Desert Climate Region & Mid Latitude Desert Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: These deserts are located in the in­terior plateau and basins in Asia and North America. They are surrounded by high mountain regions. Ti­bet and Gobi are typical examples. The main characteristic of this region is that it receives scanty rainfall as the interior location is surrounded by high mountains which prevent the inflow of moist air. Interior location results in greater extreme of temperature be­tween summer and winter. Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Mid Latitude Desert Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Mid Latitude Desert Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Mid Latitude Desert Climate Region & Mid Latitude Desert Climate Time Scale. Rep Opinion 2017;9(11s):128-130]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 43. doi:10.7537/marsroj0911s17.43.

Key Words: Mid Latitude Desert Region., Mid Latitude Desert Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale

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Basics Of Global Monsoon Time Scales Polar High Lands Ice Cape Climate Region & Polar Highlands Ice Cape Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: Antarctica and Greenland are examples of large land masses in polar regions having permanent ice caps. During summer temperature does not exceed 10°C. Precipitation is low and occurs as snowfall during winter. Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Polar Highlands Ice Cape Climate Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Polar Highlands Ice Cape Climate Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Polar High Lands Ice Cape Climate Region & Polar Highlands Ice Cape Climate Time Scale. Rep Opinion 2017;9(11s):131-133]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 44. doi:10.7537/marsroj0911s17.44.

Key Words: Polar Highlands Ice Cape Climate Region, Polar Highlands Ice Cape Climate Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale

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Basics Of Global Monsoon Time Scales Polar Low Lands Climate Region & Polar Low Lands Tundra Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: The vast lowlands, lying along the shores of Arctic Ocean, where ground is frozen for the greater part of the year are known as Tundra’s. The are low-lying cold deserts between the regions of eternal snow and ice in north and coniferous in the south. They are found in north of Asia as well as in Canada and Europe where they are known as Bar­ren lands. The region has long severe cold winter and a short cool summer. Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Polar Low Lands Tundra Climate Region which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Polar Low Lands Tundra Climate Region.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Polar Low Lands Climate Region & Polar Low Lands Tundra Climate Time Scale. Rep Opinion 2017;9(11s):134-136]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 45. doi:10.7537/marsroj0911s17.45.

Key Words: Polar Low Lands Tundra Climate Region, Polar Low Lands Tundra Climate Region, Indian Monsoon Time Scale, Global Monsoon Time Scale.

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Basics Of Global Monsoon Time Scales Taiga Coniferous Climate Region & Taiga Coniferous Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: This region occurs as a broad belt in Europe, Asia and North America between the mid latitude of grassland region in South and Polar Tun­dra in the North. The climate is cold and moist. The region has short warm summer and long cold winter. Rivers remain frozen and snow covers the ground for many months. Annual precipitation is moderate in amount with maximum during summer. Conifer­ous forests occur and contain softwood trees like oak, birch and maple. Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Taiga Coniferous Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Taiga Coniferous Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Taiga Coniferous Climate Region & Taiga Coniferous Climate Time Scale. Rep Opinion 2017;9(11s):137-139]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 46. doi:10.7537/marsroj0911s17.46.

Key Words: Taiga Coniferous Region., Taiga Coniferous Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale

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Basics Of Global Monsoon Time Scales Tropical Deciduous Forest Region & Tropical Deciduous Forest Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: This region includes eastern margins of the continents between 10°N to 30°N and 10°S to 30°S. Rainfall is moderate except in coastal regions and mountainous tracts. The summers are hot and rainy while winters are warm and dry. Parts of region such as India, south East Asia, West Africa and Northern Australia experience a typical monsoon climate having seasonal reversal of winds. Trade winds prevail in winter and monsoon winds blowing in opposite direction prevail during summer. Winds are onshore during summer. Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Tropical Deciduous Forest Climate Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Tropical Deciduous Forest Climate Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Tropical Deciduous Forest Region & Tropical Deciduous Forest Climate Time Scale. Rep Opinion 2017;9(11s):140-142]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 47. doi:10.7537/marsroj0911s17.47.

Key Words: Tropical Deciduous Forest Climate Region, Tropical Deciduous Forest Climate Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale

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Basics Of Global Monsoon Time Scales Tropical Desert Climate Region & Tropical Desert Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: Tropical deserts are located on the western margins of continents in the Trade Wind belt roughly between 20° and 30°N and S latitudes and are known as hot or trade wind deserts. Annual precipitation is generally less than 25 cm. In most of the region clear skies favour fired passage of isolation during day time and outgoing radiation from the earth during night. Therefore, the diurnal range of temperature is high. Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Tropical Desert Climate Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Tropical Desert Climate Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Tropical Desert Climate Region & Tropical Desert Climate Time Scale. Rep Opinion 2017;9(11s):143-145]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 48. doi:10.7537/marsroj0911s17.48.

Key Words: Tropical Desert Climate Region, Tropical Desert Climate Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale.

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Basics Of Global Monsoon Time Scales Tropical Grassland Savanna Region & Tropical Grassland Savanna Climate Time Scale

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad - 500 055, Telangana, India.

Email: g.r.irlapati@gmail.com

Abstract: This region lies in the interior of the continents extending up to the sea i the west in the tropical belt. It comes under the influence of equa­torial belt of calms during summer and receives convectional rainfall and it is under the influence of trade winds during winter which are dry winds and the region experiences drought. It generally lies between 5°N and 20°S latitudes. This region has moderate rainfall and greater annual range of temperature. It occurs extensively in Africa, parts of Brazilian Plateau and Orinoco basin in South America. Many studies have been conducted on the climatic conditions of the zone and invented the Global Monsoon Time Scales and Tropical Grassland Savanna Climate Time Scale which can help to estimating the past, present and future eather conditions of the zone. Researchers in the zone have to make Global Monsoon Time Scales and Tropical Grassland Savanna Climate Time Scale.

[Gangadhara Rao Irlapati. Basics Of Global Monsoon Time Scales Tropical Grassland Savanna Region & Tropical Grassland Savanna Climate Time Scale. Rep Opinion 2017;9(11s):146-148]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 49. doi:10.7537/marsroj0911s17.49.

Key Words: Tropical Grassland Savanna Climate Region, Tropical Grassland Savanna Climate Time Scale, Indian Monsoon Time Scale, Global Monsoon Time Scale

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African Tectanic Plate G.R.Irlapati’S Geoscope

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad, India-500055

Email: scientistgangadhar@gmail.com

Abstract: An earthquake zone is a region in which seismic activity is more frequent. These zones are also referred to as seismic zones and seismic hazard zones. Most high-activity earthquake danger zones are situated along the fault zones. Fault zones that are prone to seismic activity are regions of the Earth's crust. The occurrence of fault zones usually takes place in those areas where tectonic plates meet. Fault zones are also located around volcanoes. African tectonic plates is also an active seismic area. Geoscope is very useful to detect the earthquakes hence Geoscope establishments should be taken in order to capture the consequences just like earthquakes etc in the underground area of this zone. The details of the Geoscope are described below.

[Gangadhara Rao Irlapati. African Tectanic Plate G.R. Irlapati’S Geoscope. Rep Opinion 2017;9(11s):149-152]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 50. doi:10.7537/marsroj0911s17.50.

Keywords: G.R.Irlapati’s Geoscope, Earth Quakes, Local, Regional, Central Geoscope Centers: Simple, Homemade, Micro Geoscope Centers: Seismic luminescence studies, Electrogeopluse study etc.

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Alpine-Himalian Belt G.R.Irlapati’S Geoscope

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad, India-500055

Email: scientistgangadhar@gmail.com

Abstract: an earthquake zone is a region in which seismic activity is more frequent. These zones are also referred to as seismic zones and seismic hazard zones. Most high-activity earthquake danger zones are situated along the fault zones. Fault zones that are prone to seismic activity are regions of the Earth's crust. The occurrence of fault zones usually takes place in those areas where tectonic plates meet. Fault zones are also located around volcanoes. The Alpine-Himalayan belt is an active seismic zone, where almost the whole of ran is located. This makes the country susceptible to violent tremors. Geoscope is very useful to detect the earthquakes hence Geoscope establishments should be taken in order to capture the consequences just like earthquakes etc in the underground area of this zone. The details of the Geoscope are described below.

[Gangadhara Rao Irlapati. Alpine-Himalian Belt G.R.Irlapati’S Geoscope. Rep Opinion 2017;9(11s):153-156]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 51. doi:10.7537/marsroj0911s17.51.

Keywords: G.R.Irlapati’s Geoscope, Earth Quakes, Local, Regional, Central Geoscope Centers: Simple, Homemade, Micro Geoscope Centers: Seismic luminescence studies, Electrogeopluse study etc.

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Cascadia Subduction Zone G.R.Irlapati’S Geoscope

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad, India-500055

Email: scientistgangadhar@gmail.com

Abstract: An earthquake zone is a region in which seismic activity is more frequent. These zones are also referred to as seismic zones and seismic hazard zones. Most high-activity earthquake danger zones are situated along the fault zones. Fault zones that are prone to seismic activity are regions of the Earth's crust. The occurrence of fault zones usually takes place in those areas where tectonic plates meet. Fault zones are also located around volcanoes. The Cascadia Subduction Zone is a dangerous zone which can cause havoc Vancouver Portland and Seattle. Geoscope is very useful to detect the earthquakes hence Geoscope establishments should be taken in order to capture the consequences just like earthquakes etc in the underground area of this zone. The details of the Geoscope are described below.

[Gangadhara Rao Irlapati. Cascadia Subduction Zone G.R. Irlapati’S Geoscope. Rep Opinion 2017;9(11s):157-160]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 52. doi:10.7537/marsroj0911s17.52.

Keywords: G.R.Irlapati’s Geoscope, Earth Quakes, Local, Regional, Central Geoscope Centers: Simple, Homemade, Micro Geoscope Centers: Seismic luminescence studies, Electrogeopluse study etc.

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Eurasian Tectanic Plates G.R.Irlapati’S Geoscope

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad, India-500055

Email: scientistgangadhar@gmail.com

Abstract: an earthquake zone is a region in which seismic activity is more frequent. These zones are also referred to as seismic zones and seismic hazard zones Most high-activity earthquake danger zones are situated along the fault zones. Fault zones that are prone to seismic activity are regions of the Earth's crust. The occurrence of fault zones usually takes place in those areas where tectonic plates meet. Fault zones are also located around volcanoes. To its south of Italy is located the convergence of the Eurasian and African tectonic plates. Geoscope is very useful to detect the earthquakes hence Geoscope establishments should be taken in order to capture the consequences just like earthquakes etc in the underground area of this zone. The details of the Geoscope are described below.

[Gangadhara Rao Irlapati. Eurasian Tectanic Plates G.R.Irlapati’S Geoscope. Rep Opinion 2017;9(11s):161-165]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 53. doi:10.7537/marsroj0911s17.53.

Keywords: G.R. Irlapati’s Geoscope, Earth Quakes, Local, Regional, Central Geoscope Centers: Simple, Homemade, Micro Geoscope Centers: Seismic luminescence studies, Electrogeopluse study etc.

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Iranian And Arabian Micro Plates G.R.Irlapati’S Geoscope

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad, India-500055

Email: scientistgangadhar@gmail.com

Abstract: an earthquake zone is a region in which seismic activity is more frequent. These zones are also referred to as seismic zones and seismic hazard zones. Most high-activity earthquake danger zones are situated along the fault zones. Fault zones that are prone to seismic activity are regions of the Earth's crust. The occurrence of fault zones usually takes place in those areas where tectonic plates meet. Fault zones are also located around volcanoes. The meeting of the Iranian and Arabian micro-plates makes it highly prone to dangerous seismic activity. Geoscope is very useful to detect the earthquakes hence Geoscope establishments should be taken in order to capture the consequences just like earthquakes etc in the underground area of this zone. The details of the Geoscope are described below.

[Gangadhara Rao Irlapati. Iranian And Arabian Micro Plates G.R.Irlapati’S Geoscope. Rep Opinion 2017;9(11s):166-169]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 54. doi:10.7537/marsroj0911s17.54.

Keywords: G.R.Irlapati’s Geoscope, Earth Quakes, Local, Regional, Central Geoscope Centers: Simple, Homemade, Micro Geoscope Centers: Seismic luminescence studies, Electrogeopluse study etc.

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Islamabad Fault Zone G.R. Irlapati’S Geoscope

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad, India-500055

Email: scientistgangadhar@gmail.com

Abstract: an earthquake zone is a region in which seismic activity is more frequent. These zones are also referred to as seismic zones and seismic hazard zones. Most high-activity earthquake danger zones are situated along the fault zones. Fault zones that are prone to seismic activity are regions of the Earth's crust. The occurrence of fault zones usually takes place in those areas where tectonic plates meet. Fault zones are also located around volcanoes. Islamabad, capital of the Asian country of Pakistan, is located on major fault lines. The meeting of the Iranian and Arabian micro-plates makes it highly prone to dangerous seismic activity. Geoscope is very useful to detect the earthquakes hence Geoscope establishments should be taken in order to capture the consequences just like earthquakes etc in the underground area of this zone. The details of the Geoscope are described below.

[Gangadhara Rao Irlapati. Islamabad Fault Zone G.R. Irlapati’S Geoscope. Rep Opinion 2017;9(11s):170-173]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 55. doi:10.7537/marsroj0911s17.55.

Keywords: G.R.Irlapati’s Geoscope, Earth Quakes, Local, Regional, Central Geoscope Centers: Simple, Homemade, Micro Geoscope Centers: Seismic luminescence studies, Electrogeopluse study etc.

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Japan Oceanic Plate G.R. Irlapati’S Geoscope

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad, India-500055

Email: scientistgangadhar@gmail.com

Abstract: an earthquake zone is a region in which seismic activity is more frequent. These zones are also referred to as seismic zones and seismic hazard zones. Most high-activity earthquake danger zones are situated along the fault zones. Fault zones that are prone to seismic activity are regions of the Earth's crust. The occurrence of fault zones usually takes place in those areas where tectonic plates meet. Fault zones are also located around volcanoes. Japan is located on the convergence of many oceanic and continental plates. The Great Kanto earthquake in 1923, measured 8.2 magnitude on Richter scale devastated the densely populated cities of Tokyo and Yokohama, resulting in the death of 130,000 people. Geoscope is very useful to detect the earthquakes hence Geoscope establishments should be taken in order to capture the consequences just like earthquakes etc in the underground area of this zone. The details of the Geoscope are described below.

[Gangadhara Rao Irlapati. Japan Oceanic Plate G.R. Irlapati’S Geoscope. Rep Opinion 2017;9(11s):174-177]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 56. doi:10.7537/marsroj0911s17.56.

Keywords: G.R. Irlapati’s Geoscope, Earth Quakes, Local, Regional, Central Geoscope Centers: Simple, Homemade, Micro Geoscope Centers: Seismic luminescence studies, Electrogeopluse study etc

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Mexicp Zone G.R.Irlapati’S Geoscope

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad, India-500055

Email: scientistgangadhar@gmail.com

Abstract: an earthquake zone is a region in which seismic activity is more frequent. These zones are also referred to as seismic zones and seismic hazard zones. Most high-activity earthquake danger zones are situated along the fault zones. Fault zones that are prone to seismic activity are regions of the Earth's crust. The occurrence of fault zones usually takes place in those areas where tectonic plates meet. Fault zones are also located around volcanoes. Located on the convergence of three of the earth’s tectonic plates, Mexico is also prone to earthquakes and volcanic eruptions. In 1985 an earthquake on a massive scale hit Mexico resulting in 9,500 fatalities.. Geoscope is very useful to detect the earthquakes hence Geoscope establishments should be taken in order to capture the consequences just like earthquakes etc in the underground area of this zone. The details of the Geoscope are described below.

[Gangadhara Rao Irlapati. Mexicp Zone G.R.Irlapati’S Geoscope. Rep Opinion 2017;9(11s):178-181]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 57. doi:10.7537/marsroj0911s17.57.

Keywords: G.R.Irlapati’s Geoscope, Earth Quakes, Local, Regional, Central Geoscope Centers: Simple, Homemade, Micro Geoscope Centers: Seismic luminescence studies, Electrogeopluse study etc

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Missouri, The New Madrid Seismic Zone G.R. Irlapati’S Geoscope

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad, India-500055

Email: scientistgangadhar@gmail.com

Abstract: An earthquake zone is a region in which seismic activity is more frequent. These zones are also referred to as seismic zones and seismic hazard zones.  Most high-activity earthquake danger zones are situated along the fault zones. Fault zones that are prone to seismic activity are regions of the Earth's crust. The occurrence of fault zones usually takes place in those areas where tectonic plates meet. Fault zones are also located around volcanoes.  Located in Missouri, the New Madrid Seismic Zone is also an active fault.  Geoscope is very useful to detect the earthquakes hence Geoscope establishments should be taken in order to capture the consequences just like earthquakes etc in the underground area of this zone. The details of the Geoscope are described below.

[Gangadhara Rao Irlapati. Missouri, The New Madrid Seismic Zone G.R. Irlapati’S Geoscope. Rep Opinion 2017;9(11s):182-185]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 58. doi:10.7537/marsroj0911s17.58.

Keywords:  G.R. Irlapati’s Geoscope, Earth Quakes, Local, Regional, Central Geoscope Centers: Simple, Homemade, Micro Geoscope Centers: Seismic luminescence studies, Electrogeopluse study etc.

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North American And Caribbean Tectanic Plate G.R. Irlapati’S Geoscope

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad, India-500055

Email: scientistgangadhar@gmail.com

Abstract: An earthquake zone is a region in which seismic activity is more frequent. These zones are also referred to as seismic zones and seismic hazard zones. Most high-activity earthquake danger zones are situated along the fault zones. Fault zones that are prone to seismic activity are regions of the Earth's crust. The occurrence of fault zones usually takes place in those areas where tectonic plates meet. Fault zones are also located around volcanoes. North American and Caribbean tectonic plates are famous seismic zones. The San Andreas Fault zone is located in California. The Hayward fault in the San Francisco Bay area is referred to as a tectonic time bomb by U.S. Geological Survey Scientists. Geoscope is very useful to detect the earthquakes hence Geoscope establishments should be taken in order to capture the consequences just like earthquakes etc in the underground area of this zone. The details of the Geoscope are described below.

[Gangadhara Rao Irlapati. North American And Caribbean Tectanic Plate G.R. Irlapati’S Geoscope. Rep Opinion 2017;9(11s):186-189]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 59. doi:10.7537/marsroj0911s17.59.

Keywords: G.R. Irlapati’s Geoscope, Earth Quakes, Local, Regional, Central Geoscope Centers: Simple, Homemade, Micro Geoscope Centers: Seismic luminescence studies, Electrogeopluse study etc.

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Padang Fault Zone G.R. Irlapati’S Geoscope

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad, India-500055

Email: scientistgangadhar@gmail.com

Abstract: an earthquake zone is a region in which seismic activity is more frequent. These zones are also referred to as seismic zones and seismic hazard zone. Most high-activity earthquake danger zones are situated along the fault zones. Fault zones that are prone to seismic activity are regions of the Earth's crust. The occurrence of fault zones usually takes place in those areas where tectonic plates meet. Fault zones are also located around volcanoes. Padang, the capital of West Sumatra province of Indonesia’s, is located on some of the world’s most dangerous fault zones. Geoscope is very useful to detect the earthquakes hence Geoscope establishments should be taken in order to capture the consequences just like earthquakes etc in the underground area of this zone. The details of the Geoscope are described below.

[Gangadhara Rao Irlapati. Padang Fault Zone G.R. Irlapati’S Geoscope. Rep Opinion 2017;9(11s):190-193]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 60. doi:10.7537/marsroj0911s17.60.

Keywords: G.R. Irlapati’s Geoscope, Earth Quakes, Local, Regional, Central Geoscope Centers: Simple, Homemade, Micro Geoscope Centers: Seismic luminescence studies, Electrogeopluse study etc

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Xianshuihe, Min Jiang And Kunlun Fault Lines G.R. Irlapati’S Geoscope

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad, India-500055

Email: scientistgangadhar@gmail.com

Abstract: an earthquake zone is a region in which seismic activity is more frequent. These zones are also referred to as seismic zones and seismic hazard zones. Most high-activity earthquake danger zones are situated along the fault zones. Fault zones that are prone to seismic activity are regions of the Earth's crust. The occurrence of fault zones usually takes place in those areas where tectonic plates meet. Fault zones are also located around volcanoes. The Xianshuihe, Min Jiang and Kunlun fault lines in China can produce disaster. Geoscope is very useful to detect the earthquakes hence Geoscope establishments should be taken in order to capture the consequences just like earthquakes etc in the underground area of this zone. The details of the Geoscope are described below.

[Gangadhara Rao Irlapati. Xianshuihe, Min Jiang And Kunlun Fault Lines G.R. Irlapati’S Geoscope. Rep Opinion 2017;9(11s):194-197]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 61. doi:10.7537/marsroj0911s17.61.

Keywords: G.R.Irlapati’s Geoscope, Earth Quakes, Local, Regional, Central Geoscope Centers: Simple, Homemade, Micro Geoscope Centers: Seismic luminescence studies, Electrogeopluse study etc

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Africa Continental Seismic Zone G.R. Irlapati’S Geoscope

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad, India-500055

Email: scientistgangadhar@gmail.com

Abstract: Africa has far fewer earthquake zones than other continents, with little to no activity across much of the Sahara and central part of the continent. There are pockets of activity, however. The eastern Mediterranean coast, particularly Lebanon, is one noteworthy region. There, the Arabian plate collides with the Eur-Asian and African plates. The region near the Horn of Africa is another active area. One of the most powerful African earthquakes in recorded history occurred in December 1910, when a 7.8 quake struck western Tanzania. Geoscope is very useful to detect the earthquakes hence Geoscope establishments should be taken in order to capture the consequences just like earthquakes etc in the underground area of this zone. The details of the Geoscope are described below.

[Gangadhara Rao Irlapati. Africa Continental Seismic Zone G.R. Irlapati’S Geoscope. Rep Opinion 2017;9(11s):198-201]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 62. doi:10.7537/marsroj0911s17.62.

Keywords: G.R. Irlapati’s Geoscope, Earth Quakes, Local, Regional, Central Geoscope Centers: Simple, Homemade, Micro Geoscope Centers: Seismic luminescence studies, Electrogeopluse study etc.

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Antarctica Continental Seismic Zone G.R. Irlapati’S Geoscope

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad, India-500055

Email: scientistgangadhar@gmail.com

Abstract: compared with the other six continents, Antarctica is the least active in terms of earthquakes. Part of this is because very little of its land mass lies on or near the intersection of continental plates. One exception is the region around Tierra del Fuego in South America, where the Antarctic plate meets the Scotia plate. Antarctica's biggest quake, a magnitude 8.1 event, occurred in 1998 in the Balleny Islands, which are south of New Zealand. But in general, Antarctica is seismically quiet. Geoscope is very useful to detect the earthquakes hence Geoscope establishments should be taken in order to capture the consequences just like earthquakes etc in the underground area of this zone. The details of the Geoscope are described below.

[Gangadhara Rao Irlapati. Antarctica Continental Seismic Zone G.R. Irlapati’S Geoscope. Rep Opinion 2017;9(11s):202-205]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 63. doi:10.7537/marsroj0911s17.63.

Keywords: G.R. Irlapati’s Geoscope, Earth Quakes, Local, Regional, Central Geoscope Centers: Simple, Homemade, Micro Geoscope Centers: Seismic luminescence studies, Electrogeopluse study etc

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Asia Continental Seismic Zone G.R. Irlapati’S Geoscope

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad, India-500055

Email: scientistgangadhar@gmail.com

Abstract: Asia is a hotbed of earthquake activity, particularly where the Australian plate wraps around the Indonesian archipelago, and again in Japan, which lies astride three continental plates. More earthquakes are recorded in Japan than any other place on earth. The nations of Indonesia, Fiji and Tonga also experience record numbers of earthquakes annually. When a 9.1. quake struck the western coast of Sumatra in 2014, it generated the largest tsunami in recorded history.

More than 200,000 people died in the resulting inundation. Other major historical quakes include a 9.0 quake on Russia's Kamchatka Peninsula in 1952 and an 8.6 magnitude quake that struck Tibet in 1950. Scientists as far away as Norway felt that quake.

Central Asia is another of the world's major earthquake zones. The greatest activity occurs along a swath of territory extending from the eastern shores of the Black Sea, down through Iran and its border with Pakistan and along the southern shores of the Caspian Sea. 

Geoscope is very useful to detect the earthquakes hence Geoscope establishments should be taken in order to capture the consequences just like earthquakes etc in the underground area of this zone. The details of the Geoscope are described below.

[Gangadhara Rao Irlapati. Asia Continental Seismic Zone G.R. Irlapati’S Geoscope. Rep Opinion 2017;9(11s):206-209]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 64. doi:10.7537/marsroj0911s17.64.

Keywords: G.R. Irlapati’s Geoscope, Earth Quakes, Local, Regional, Central Geoscope Centers: Simple, Homemade, Micro Geoscope Centers: Seismic luminescence studies, Electrogeopluse study etc

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Australasian Continental Seismic Zone G.R. Irlapati’S Geoscope

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad, India-500055

Email: scientistgangadhar@gmail.com

Abstract: Australia and New Zealand are a study in seismic contrast. While the continental of Australia has a low to moderate risk of quakes overall, its smaller island neighbor is another of the world's earthquake hot spots. New Zealand's most powerful temblor stuck in 1855 and measured 8.2 on the Richter scale. According to historians, the Wairarapa quake thrust some parts of the landscape 20 feet higher in elevation. Geoscope is very useful to detect the earthquakes hence Geoscope establishments should be taken in order to capture the consequences just like earthquakes etc in the underground area of this zone. The details of the Geoscope are described below.

[Gangadhara Rao Irlapati. Australasian Continental Seismic Zone G.R. Irlapati’S Geoscope. Rep Opinion 2017;9(11s):210-213]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 65. doi:10.7537/marsroj0911s17.65.

Keywords: G.R. Irlapati’s Geoscope, Earth Quakes, Local, Regional, Central Geoscope Centers: Simple, Homemade, Micro Geoscope Centers: Seismic luminescence studies, Electrogeopluse study etc

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Europe Continental Seismic Zone G.R. Irlapati’S Geoscope

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad, India-500055

Email: scientistgangadhar@gmail.com

Abstract: northern europe is largely free of major earthquake zones, except for a region centered around western Iceland known also for its volcanic activity. The risk of seismic activity increases as you move southeast toward Turkey and along portions of the Mediterranean coast. In both instances, the quakes are caused by the African continental plate where it jabs upward into the Eurasian plate beneath the Adriatic Sea. The Portuguese capital of Lisbon was practically leveled in 1755 by a magnitude 8.7 quake, one of the strongest ever recorded. Central Italy and western Turkey are also epicenters of quake activity. Geoscope is very useful to detect the earthquakes hence Geoscope establishments should be taken in order to capture the consequences just like earthquakes etc in the underground area of this zone. The details of the Geoscope are described below.

[Gangadhara Rao Irlapati. Europe Continental Seismic Zone G.R. Irlapati’S Geoscope. Rep Opinion 2017;9(11s):214-217]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 66. doi:10.7537/marsroj0911s17.66.

Keywords: G.R. Irlapati’s Geoscope, Earth Quakes, Local, Regional, Central Geoscope Centers: Simple, Homemade, Micro Geoscope Centers: Seismic luminescence studies, Electrogeopluse study etc

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North American Continental Seismic Zone G.R. Irlapati’S Geoscope

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad, India-500055

Email: scientistgangadhar@gmail.com

Abstract: there are several major earthquake zones in North America. One of the most notable can be found on Alaska's central coast, extending north to Anchorage and Fairbanks. In 1964, one of the most powerful earthquakes in modern history, measuring 9.2 on the Richter scale, struck Prince William Sound in Alaska.

Another zone of activity stretches along the coast from British Columbia to Baja Mexico where the Pacific plate rubs against the North American plate. California's Central Valley, San Francisco Bay Area and much of Southern California are crisscrossed with active fault lines that have spawned a number of notable quakes, including the magnitude 7.7 temblor that helped level San Francisco in 1906.

In Mexico, an active quake zone follows the western Sierras south from near Puerta Vallarta to the Pacific coast at the Guatemala border. In fact, most of the western coast of Central America is seismically active as the Cocos plate rubs against the Caribbean plate. The eastern edge of North America is quiet by comparison, though there is a small zone of activity near the entry to the St. Lawrence River in Canada.

Other areas of lesser earthquake activity include the New Madrid fault region where the Mississippi and Ohio Rivers converge near Missouri, Kentucky and Illinois. Another region forms an arc from Jamaica to southeastern Cuba and across Haiti and the Dominican Republic.

Geoscope is very useful to detect the earthquakes hence Geoscope establishments should be taken in order to capture the consequences just like earthquakes etc in the underground area of this zone. The details of the Geoscope are described below.

[Gangadhara Rao Irlapati. North American Continental Seismic Zone G.R. Irlapati’S Geoscope. Rep Opinion 2017;9(11s):218-221]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 67. doi:10.7537/marsroj0911s17.67.

Keywords: G.R. Irlapati’s Geoscope, Earth Quakes, Local, Regional, Central Geoscope Centers: Simple, Homemade, Micro Geoscope Centers: Seismic luminescence studies, Electrogeopluse study etc.

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South American Continental Seismic Zone G.R. Irlapati’S Geoscope

Gangadhara Rao Irlapati

H.No.5-30-4/1, Saibabanagar, Jeedimetla, Hyderabad, India-500055

Email: scientistgangadhar@gmail.com

Abstract: south america's most active earthquake zones stretch the length of the continent's Pacific border. A second notable seismic region runs along the Caribbean coast of Colombia and Venezuela. This activity is due to a number of continental plates colliding with the South American plate. Four of the 10 strongest earthquakes recorded have occurred in South America.

In fact, the most powerful earthquake ever recorded took place in central Chile in May 1960, when a magnitude 9.5 quake hit near Saavedra. More than 2 million people were left homeless and almost 5,000 killed. A half century later, a magnitude 8.8 temblor struck nearby in the city of Concepcion in 2010. About 500 people died and 800,000 were left homeless, and the nearby Chilean capital of Santiago sustained serious damage in some areas.

Geoscope is very useful to detect the earthquakes hence Geoscope establishments should be taken in order to capture the consequences just like earthquakes etc in the underground area of this zone. The details of the Geoscope are described below.

[Gangadhara Rao Irlapati. South American Continental Seismic Zone G.R. Irlapati’S Geoscope. Rep Opinion 2017;9(11s):222-225]. ISSN 1553-9873 (print); ISSN 2375-7205 (online). http://www.sciencepub.net/report. 68. doi:10.7537/marsroj0911s17.68.

Keywords: G.R. Irlapati’s Geoscope, Earth Quakes, Local, Regional, Central Geoscope Centers: Simple, Homemade, Micro Geoscope Centers: Seismic luminescence studies, Electrogeopluse study etc

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Maps

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