降水
环境科学
水分
打
含水量
北半球
气候学
大气科学
大气(单位)
气候模式
联轴节(管道)
气候变化
气象学
地质学
数学
地理
工程类
海洋学
算术
机械工程
岩土工程
作者
Randal D. Koster,Paul A. Dirmeyer,Zhichang Guo,Gordon B. Bonan,Ed Chan,Peter M. Cox,Chris Gordon,Shinjiro Kanae,Eva Kowalczyk,David M. Lawrence,Ping Liu,Cheng‐Hsuan Lu,Sergey Malyshev,B. J. McAvaney,Ken Mitchell,David M. Mocko,Taikan Oki,Keith W. Oleson,A. J. Pitman,Y. C. Sud
出处
期刊:Science
[American Association for the Advancement of Science]
日期:2004-08-20
卷期号:305 (5687): 1138-1140
被引量:2737
标识
DOI:10.1126/science.1100217
摘要
Previous estimates of land-atmosphere interaction (the impact of soil moisture on precipitation) have been limited by a lack of observational data and by the model dependence of computational estimates. To counter the second limitation, a dozen climate-modeling groups have recently performed the same highly controlled numerical experiment as part of a coordinated comparison project. This allows a multimodel estimation of the regions on Earth where precipitation is affected by soil moisture anomalies during Northern Hemisphere summer. Potential benefits of this estimation may include improved seasonal rainfall forecasts.
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