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Greenbelt - Nov 06, 2002 Warmer or colder sea surface temperatures (SST) may affect one of the world's key large-scale atmospheric circulations that regulate the intensity and breaking of rainfall associated with the South Asian and Australian monsoons, according to new research from NASA. A monsoon is a wind that changes direction with the seasons. Monsoons develop from changing patterns of atmospheric circulation which are caused by changes in heating and cooling of land and oceans. One of the strongest and most well-known monsoons is the one which affects India and Southeast Asia in June through September. The summer monsoon blows southwesterly across the Indian Ocean and is extremely wet. During the summer monsoon, particularly in July, there is usually a break period in the monsoon, when the rains stop and re-start. A phenomenon known as the Madden Julian Oscillation (MJO) has been found to affect that break and the variation of the MJO is affected by the variation of the SSTs. The MJO is the main fluctuation of atmospheric circulation that explains variations of weather in the tropics and that regulates south Asian monsoons. The variation of the MJO involves variations in wind, SST, cloudiness, and rainfall. The MJO can be characterized by a large-scale eastward movement of air in the upper troposphere with a period of about 20-70 days, over the tropical eastern Indian and western Pacific Oceans at approximately 7.5 miles (200 millibars) high in the atmosphere. Man Li Wu, a researcher from NASA's Goddard Space Flight Center in Greenbelt, Md., and lead author of the study, used computer models that simulate the atmosphere in the region. One of the purposes of this study is to examine to what extent intra-seasonal SST variations affect the MJO. "Changes in SSTs will affect a large scale atmospheric circulation known as the MJO in the area of southern Asia, which regulates the variability of the monsoon," Wu said.
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