THE EFFECT OF LAND-SEA CONTRAST ON INTERANNUAL VARIABILITY OF THE ASIAN MONSOON*

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* “National Key Programme for Developing Basic Sciences”G 1998040900 Part Ⅰ.

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    Abstract

  • Abstract

    Values of the net radiative heating(QRT)at the top of atmosphere(TOA) are derived from the satellite-observed outgoing long wave radiation(OLR)and the TOA short wave net irradiance (SHT) for the region of the Tibetan Plateau and surrounding areas(40°S-40°N,0-180°E)and the period of months from January 1979 to December 1988.The anomalous QRT(QRTA)in relation to the interannual variability of Asian monsoon is discussed.QRTA for the earth-atmosphere system in the domain may be linked to the thermal contrasts between continents and oceans and between the plateau and surrounding free atmosphere.
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