Current changes in tropical precipitation

被引:196
作者
Allan, Richard P. [1 ]
Soden, Brian J. [2 ]
John, Viju O. [3 ]
Ingram, William [3 ,4 ]
Good, Peter [3 ]
机构
[1] Univ Reading, Dept Meteorol, Reading RG6 6BB, Berks, England
[2] Univ Miami, Rosenstiel Sch Marine & Atmospher Sci, Div Meteorol & Phys Oceanog, Miami, FL 33149 USA
[3] Met Off, Exeter EX1 3PB, Devon, England
[4] Univ Oxford, Dept Phys, Oxford OX1 3PU, England
基金
英国自然环境研究理事会;
关键词
global water cycle; satellite data; climate models; rainfall extremes; trends; climate change; EXTREME PRECIPITATION; CLIMATE; INCREASES; TEMPERATURE;
D O I
10.1088/1748-9326/5/2/025205
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Current changes in tropical precipitation from satellite data and climate models are assessed. Wet and dry regions of the tropics are defined as the highest 30% and lowest 70% of monthly precipitation values. Observed tropical ocean trends in the wet regime (1.8%/decade) and the dry regions (-2.6%/decade) according to the Global Precipitation Climatology Project (GPCP) over the period including Special Sensor Microwave Imager (SSM/I) data (1988-2008), where GPCP is believed to be more reliable, are of smaller magnitude than when including the entire time series (1979-2008) and closer to model simulations than previous comparisons. Analysing changes in extreme precipitation using daily data within the wet regions, an increase in the frequency of the heaviest 6% of events with warming for the SSM/I observations and model ensemble mean is identified. The SSM/I data indicate an increased frequency of the heaviest events with warming, several times larger than the expected Clausius-Clapeyron scaling and at the upper limit of the substantial range in responses in the model simulations.
引用
收藏
页数:7
相关论文
共 41 条
[41]   Detection of human influence on twentieth-century precipitation trends [J].
Zhang, Xuebin ;
Zwiers, Francis W. ;
Hegerl, Gabriele C. ;
Lambert, F. Hugo ;
Gillett, Nathan P. ;
Solomon, Susan ;
Stott, Peter A. ;
Nozawa, Toru .
NATURE, 2007, 448 (7152) :461-U4