Contribution of ocean overturning circulation to tropical rainfall peak in the Northern Hemisphere

被引：1
|
作者：
Dargan M. W. Frierson
Yen-Ting Hwang
Neven S. Fučkar
Richard Seager
Sarah M. Kang
Aaron Donohoe
Elizabeth A. Maroon
Xiaojuan Liu
David S. Battisti
机构：
[1] University of Washington,Department of Atmospheric Sciences
[2] International Pacific Research Center,Department of Earth
[3] University of Hawaii,undefined
[4] Institut Català de Ciències del Clima,undefined
[5] Lamont-Doherty Earth Observatory of Columbia University,undefined
[6] School of Urban and Environmental Engineering,undefined
[7] Ulsan National Institute of Science and Technology,undefined
[8] Atmospheric,undefined
[9] and Planetary Sciences,undefined
[10] Massachusetts Institute of Technology,undefined
来源：
Nature Geoscience | 2013年 / 6卷
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摘要：
In the tropics, substantially more rain falls just north of the Equator. An analysis of satellite observations, reanalysis data and model simulations suggests that the meridional ocean overturning circulation contributes significantly to the tropical rainfall peak north of the Equator.
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页码：940 / 944
页数：4
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