GSTDTAP  > 气候变化
DOI10.1029/2018GL079423
Increased Frequency of Extreme Tropical Deep Convection: AIRS Observations and Climate Model Predictions
Aumann, Hartmut H.1; Behrangi, Ali1,2; Wang, Yuan1,3
2018-12-28
发表期刊GEOPHYSICAL RESEARCH LETTERS
ISSN0094-8276
EISSN1944-8007
出版年2018
卷号45期号:24页码:13530-13537
文章类型Article
语种英语
国家USA
英文摘要

Atmospheric Infrared Sounder (AIRS) data from the tropical oceans (30 degrees N to 30 degrees S) are used to derive the probability of the process resulting in deep convective clouds (DCCs) as function of the sea surface temperature (SST). For DCC at or below the tropopause the onset temperature of this process shifts at the same rate as the increase in the mean SST. For tropopause overshooting DCC, which are associated with extreme rain events, the shift of the onset temperature is slower, causing their frequency to increase by about 21%/K of warming of the oceans. This sensitivity is not inconsistent with the sensitivity of the increase of extreme deep convective rain in the National Center for Atmospheric Research Community Atmosphere Model version 5 model for a warmer SST. The mean of the 36 fifth Phase of the Coupled Model Intercomparison Project models predicts a 2.7 K warmer tropical SST by the end of this century, resulting in a 60% increases in the frequency of tropopause overshooting DCC.


Plain Language Summary We use 15 years of Atmospheric Infrared Sounder observations of the tropical oceans to derive the probability of the deep convective cloud (DCC) process as a function of the sea surface temperature. Based on this, the frequency of extreme (tropopause overshooting) DCCs will increase about 21% per 1 K of warming of the tropical oceans. Tropopause overshooting DCC are correlated with extreme rain rates. We evaluated the expected increase in the frequency of extreme precipitation in the National Center for Atmospheric Research Community Atmosphere Model version 5 model in a warmer tropical ocean. The increase of extreme rain rates in the model is consistent with the Atmospheric Infrared Sounder-derived increase in frequency of extreme DCC. The mean of the fifth Phase of the Coupled Model Intercomparison Project models predicts a 2.7 K increase in the surface temperature of the tropical oceans by the end of this century. This means that the frequency of extreme DCC in the tropical oceans could increase by about 60%.


英文关键词climate sensitivity severe storms AIRS climate models
领域气候变化
收录类别SCI-E
WOS记录号WOS:000456404600039
WOS关键词SYSTEM MODEL ; CLOUD ; RESOLUTION ; RAINFALL
WOS类目Geosciences, Multidisciplinary
WOS研究方向Geology
引用统计
文献类型期刊论文
条目标识符http://119.78.100.173/C666/handle/2XK7JSWQ/27037
专题气候变化
作者单位1.CALTECH, Jet Prop Lab, Pasadena, CA 91125 USA;
2.Univ Arizona, Dept Hydrol & Atmospher Sci, Tucson, AZ USA;
3.CALTECH, Div Geol & Planetary Sci, Pasadena, CA 91125 USA
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GB/T 7714
Aumann, Hartmut H.,Behrangi, Ali,Wang, Yuan. Increased Frequency of Extreme Tropical Deep Convection: AIRS Observations and Climate Model Predictions[J]. GEOPHYSICAL RESEARCH LETTERS,2018,45(24):13530-13537.
APA Aumann, Hartmut H.,Behrangi, Ali,&Wang, Yuan.(2018).Increased Frequency of Extreme Tropical Deep Convection: AIRS Observations and Climate Model Predictions.GEOPHYSICAL RESEARCH LETTERS,45(24),13530-13537.
MLA Aumann, Hartmut H.,et al."Increased Frequency of Extreme Tropical Deep Convection: AIRS Observations and Climate Model Predictions".GEOPHYSICAL RESEARCH LETTERS 45.24(2018):13530-13537.
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