| CHARACTERISTICS OF THE SURFACE AND ATMOSPHERIC HEATING FIELDS OVER QINGHAI-XIZANG PLATEAU FOR THE PERIOD FROM AUGUST 1982 TO JULY 1983 |
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| 作者姓名： | Ji Guoliang Pu Ming |
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| 作者单位： | Lanzhou Institute of Plateau Atmospheric Physics Academia Sinica，Lanzhou，Mianyang Weather Service，Mianyang，Sichuan Province |
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| 摘 要： | The surface and atmospheric heating fields over the Qinghai-Xizang Plateau are computed by using theobservational data of solar radiation during 1982—1983.The mian results are as follows:The central andnorthern parts of the Plateau act as heat sinks in winter from November to January.Both eastern and south-ern parts of the Plateau are of heat sources.In summer,the main part of the Plateau acts as a strong heatsource,and the center of the heating field is in the southeastern Plateau.However the main part of thePlateau acts as a heat sink for the atmospheric heating fields from October to March.The maximum intensityof the atmospheric heat sink over the central Plateau appears in December and January.From April toSeptember,the main part of the Plateau acts as a heat source for the atmospheric heating fields.
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| 收稿时间： | 2/6/1988 12:00:00 AM |
CHARACTERISTICS OF THE SURFACE AND ATMOSPHERIC HEATING FIELDS OVER QINGHAI-XIZANG PLATEAU FOR THE PERIOD FROM AUGUST 1982 TO JULY 1983 |
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| Ji Guoliang,Pu Ming.CHARACTERISTICS OF THE SURFACE AND ATMOSPHERIC HEATING FIELDS OVER QINGHAI-XIZANG PLATEAU FOR THE PERIOD FROM AUGUST 1982 TO JULY 1983[J].Acta Meteorologica Sinica,1989,3(2):228-241. |
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| Authors: | Ji Guoliang and Pu Ming |
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| Institution: | Lanzhou Institute of Plateau Atmospheric Physics, Academia Sinica, Lanzhou;Mianyang Weather Service, Mianyang, Sichuan Province |
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| Abstract: | The surface and atmospheric heating fields over the Qinghai-Xizang Plateau are computed by using the observational data of solar radiation during 1982-1983.The mian results are as follows:The central and northern parts of the Plateau act as heat sinks in winter from November to January.Both eastern and southern parts of the Plateau are of heat sources.In summer,the main part of the Plateau acts as a strong heat source,and the center of the heating field is in the southeastern Plateau.However the main part of the Plateau acts as a heat sink for the atmospheric heating fields from October to March.The maximum intensity of the atmospheric heat sink over the central Plateau appears in December and January.From April to September,the main part of the Plateau acts as a heat source for the atmospheric heating fields. |
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