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青藏高原云对地气系统短波吸收辐射强迫的气候研究
引用本文:刘艳,翁笃鸣.青藏高原云对地气系统短波吸收辐射强迫的气候研究[J].南京气象学院学报,2000,23(1):124-129.
作者姓名:刘艳  翁笃鸣
作者单位:南京气象学院环境科学系,南京,210044
基金项目:国家攀登 B项目!“青藏高原第二次科学试验”资助
摘    要:利用地球辐射平衡试验(ERBE)和国际卫星云气候计划(ESCCP)提供的总云量、得星反射率资料,计算并分析了青藏高原地气系统年、月平均云对太阳短波吸收辐射的强迫,揭示了其与总云量的关系。结果表明:高原的短事射云强迫与总云量有较好的非线性相关,呈幂指数形式,且季节变化明显;短波辐射云强迫的地理分布与高原云的分产好,高原主体和北部是短波辐射云强迫的低值区,高原东南部和西部边缘迎风部位为强迫的高值区。

关 键 词:青藏高原  地气系统  短波吸收辐射  辐射强迫  
修稿时间:1999-04-08

Climatology of cloud effects on earth-atmosphere absorbed shortwave radiation forcing over Qinghai-Tibet Plateau
LIU Yan,WENG Du-ming.Climatology of cloud effects on earth-atmosphere absorbed shortwave radiation forcing over Qinghai-Tibet Plateau[J].Journal of Nanjing Institute of Meteorology,2000,23(1):124-129.
Authors:LIU Yan  WENG Du-ming
Abstract:In terms of data provided by ERBE and ISCCP, effects of total cloudiness on earth atmosphere system absorbed shortwave cloud radiation forcing (SWCRF) are investigated over Qinghai Tibet Plateau on an annual and a monthly basis separately. It turns out that there is a good power law correlation between them,and both have obvious seasonal variations. The SWCRF's geographical distribution accords well with that of the total cloudiness over the region and its value is lower over the main and north parts, and higher over the south east part and the windward side of the west edge.
Keywords:Qinghai Tibet Plateau  earth atmosphere system  absorbed shortwave radiation  cloud radiation forcing
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