中国地表净辐射的气候学研究
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A CLIMATOLOGICAL STUDY OF THE SURFACE NET RADIATION OVER CHINA
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    摘要:

    本文根据作者提出的净辐射各分量的气候学计算方法,计算出全国223站的净辐射及其各分量的通量密度,并分析其在全国的分布特征。指出青藏高原南部雅鲁藏布江流域、内蒙高原东部为稳定的高中心,川黔山地为低中心。随着季节转移,地表净辐射分布形势有所变动。各地净辐射年变化曲线形式,特别是最大值出现月份与雨季出现早晚有很大关系。辐射平衡各分量的相对计算误差分别为:总辐射2.7%;地表反射率4.0%;有效辐射9.4%;净辐射8.9%。

    Abstract:

    Based on the climatological calculating methods proposed in this paper, the net radiation, as well as the components of radiation balance, is computed for 223 stations throughout China and their distribution patterns are analyzed graphically. It is found that high-value centers of net radiation appear steadily in both the south of the Qinghai-Tibetan Plateau and the east of Inner-Mongolia while low-value centers in the Sichuan Guizhou Plateau. Annual variation patterns of net radiation in different places, especially the month when the peak value occurs, are closely associated with the coming time of the rainy season. The components of net radiation obtained from calculation have relative errors, on the average, of 2.7% for the global radiation, 4.0% for the surface albedo, 9.4% for the effective radiation, and 8.9% for the net radiation, respectively.

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翁笃呜,孙治安,史兵,1988.中国地表净辐射的气候学研究[J].大气科学学报,11(2):132-143. Weng Duming, Sun Zhi’an, Shi Bing,1988. A CLIMATOLOGICAL STUDY OF THE SURFACE NET RADIATION OVER CHINA[J]. Trans Atmos Sci,11(2):132-143.

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  • 收稿日期:1987-05-06
  • 最后修改日期:1987-09-02
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