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青藏高原雪盖与冬季地表净辐射

COMPUTATION OF NET RADIATION OVER THE QINGHAI-XIZANG PLATEAU IN WINTER UNDER SNOW COVER

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【作者】 曹梅盛

【Author】 CAO Mei-sheng (Lanzhou Institute of Glaciology and Geocryology, Chinese Academy of Sciences, Lanzhou,Gansu 730000)

【机构】 中国科学院兰州冰川冻土研究所

【摘要】 根据青藏高原地区SMMR遥感监测雪深分布图、雪面反照率随雪深变化规律以及1982~1983年高原地表辐射平衡观测总结的有关辐射平衡分量气候学计算方法,以旬及0.5°×0.5°经纬度网格的时空高分辨率计算了高原主体1978/1979年至1986/1987年9年冬季(11~2月)地表净辐射的时间序列。结果表明,当月均日照百分率为0.73,雪盖率超过60%时,高原主体12月份地表净辐射均值已由正转负。

【Abstract】 Based on the charts of snow depth over the Qinghai-Xizang Plateau monitored by SMMR,the evolution of snow albedo with its depth and the algorithms of climatic computation on the components of radiation balance, which were summed up based on the data measured at the heat sources observation stations on the Plateau from September 1982 to August 1983, the surface net radiation over main of the Plateau was calculated at temporary and spatial resolution on dekad and 0.5° ×0.5° latitude-longitude cell, respectively, for November to February during 1978/1979 to 1986/1987. The results show that it will be altered from positive to negative in December, while the monthly mean of sunshine percentage is 73 and the snow cover percentage over 60.

【基金】 中国科学院“冰冻圈动态变化基础研究”项目
  • 【文献出处】 高原气象 ,PLATEAU METEOROLOGY , 编辑部邮箱 ,1998年04期
  • 【分类号】P422.4
  • 【被引频次】5
  • 【下载频次】184
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