East asian monsoons

By using this site, you agree to the Terms of Use and Privacy Policy. This cold and dry winter monsoon is responsible for the aeolian dust deposition and pedogenesis that resulted in the creation of the Loess Plateau. This crowds city slums and aggravates the infrastructure and sustainability of city life. First observed by World War II pilots, they develop just below the tropopause over areas of steep pressure gradient on the surface. Southern oscillation , a phenomenon first observed by Sir Gilbert Thomas Walker , director general of observatories in India, refers to the seesaw relationship of atmospheric pressures between Tahiti and Darwin , Australia. Changes in pressure over the southern oceans also affect the monsoons. This results in the north-to-south flow of the winds in the form of the northeast monsoon.
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East Asian Monsoon

The fifth condition develops during the summer due to the movement of the westerly jet streams to the north of the Himalayas and the presence of the tropical easterly jet stream over the Indian Peninsula. But with the advent of globalization, such travel is gaining popularity. The down side however is that when monsoon rains are weak, crop production is low leading to higher food prices with limited supply. The economic significance of the monsoon is aptly described by Pranab Mukherjee 's remark that the monsoon is the "real finance minister of India". The monsoon winds encounter various atmospheric conditions on their way and hence are pulsating in nature, and not steady.
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Monsoon of South Asia

This periodic change in pressure conditions is known as the Southern Oscillation, or SO. By mid-October, it withdraws completely from the northern half of the peninsula. The withdrawal takes place progressively from north to south from the first week of December to the first week of January. Orographic barriers force wind to rise. The department has tried to forecast the monsoon for India since , [40] and is the only official agency entrusted with making public forecasts about the quantity, distribution, and timing of the monsoon rains. In , IMD substantially changed its forecast methodology, model, [43] and administration. Webarchive template wayback links Use dmy dates from March Wikipedia articles needing clarification from March All articles with unsourced statements Articles with unsourced statements from July Commons category link is on Wikidata Commons category link is locally defined. As the Tibetan Plateau heats up, the low pressure created over it pulls the westerly jet north.
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Description:The retreating monsoon winds move over the Arabian Sea and the Bay of Bengal, and collect moisture on the way. But with the advent of globalization, such travel is gaining popularity. Since the Great Famine of —78 in India, various attempts have been made to predict monsoon rainfall. Also known as the thermal theory or the differential heating of sea and land theory , the traditional theory portrays the monsoon as a large-scale sea breeze. Various atmospheric conditions influence the monsoon winds. In the past, Indians usually refrained from traveling during monsoons for practical as well as religious reasons.

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