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Current changes in tropical precipitation
被引:194
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
来源:
ENVIRONMENTAL RESEARCH LETTERS
|
2010年
/
5卷
/
02期
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.
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