globalchange  > 气候减缓与适应
DOI: 10.1002/grl.50956
论文题名:
Impact of soil moisture-climate feedbacks on CMIP5 projections: First results from the GLACE-CMIP5 experiment
作者: Seneviratne S.I.; Wilhelm M.; Stanelle T.; Van Den Hurk B.; Hagemann S.; Berg A.; Cheruy F.; Higgins M.E.; Meier A.; Brovkin V.; Claussen M.; Ducharne A.; Dufresne J.-L.; Findell K.L.; Ghattas J.; Lawrence D.M.; Malyshev S.; Rummukainen M.; Smith B.
刊名: Geophysical Research Letters
ISSN: 0094-8500
EISSN: 1944-8231
出版年: 2013
卷: 40, 期:19
起始页码: 5212
结束页码: 5217
语种: 英语
英文关键词: climate extremes ; CMIP5 ; feedbacks ; land-atmosphere interactions ; projections ; soil moisture
Scopus关键词: Climate extremes ; CMIP5 ; Extreme temperatures ; Land-atmosphere interactions ; Mediterranean region ; Model inter comparisons ; Northern Hemispheres ; projections ; Earth (planet) ; Evaporative cooling systems ; Experiments ; Feedback ; Soil moisture ; Climate models ; climate effect ; climate feedback ; climate modeling ; comparative study ; evaporation ; Mediterranean environment ; Northern Hemisphere ; precipitation (climatology) ; simulation ; soil moisture ; twenty first century
英文摘要: The Global Land-Atmosphere Climate Experiment-Coupled Model Intercomparison Project phase 5 (GLACE-CMIP5) is a multimodel experiment investigating the impact of soil moisture-climate feedbacks in CMIP5 projections. We present here first GLACE-CMIP5 results based on five Earth System Models, focusing on impacts of projected changes in regional soil moisture dryness (mostly increases) on late 21st century climate. Projected soil moisture changes substantially impact climate in several regions in both boreal and austral summer. Strong and consistent effects are found on temperature, especially for extremes (about 1-1.5 K for mean temperature and 2-2.5 K for extreme daytime temperature). In the Northern Hemisphere, effects on mean and heavy precipitation are also found in most models, but the results are less consistent than for temperature. A direct scaling between soil moisture-induced changes in evaporative cooling and resulting changes in temperature mean and extremes is found in the simulations. In the Mediterranean region, the projected soil moisture changes affect about 25% of the projected changes in extreme temperature. Key Points GLACE-CMIP5 quantifies soil moisture feedbacks in climate projections Impacts on late 21st century temperature and precipitation mean and extremes Effects of about 25% for temperature extremes in Mediterranean region © 2013 The Authors. Geophysical Research Letters published by Wiley on behalf of the American Geophysical Union.
URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84884788919&doi=10.1002%2fgrl.50956&partnerID=40&md5=a2c17be27b3bbe24d8dd631e22156e4e
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/5764
Appears in Collections:气候减缓与适应

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作者单位: Institute for Atmospheric and Climate Science, ETH Zurich, CH-8092 Zurich, Switzerland

Recommended Citation:
Seneviratne S.I.,Wilhelm M.,Stanelle T.,et al. Impact of soil moisture-climate feedbacks on CMIP5 projections: First results from the GLACE-CMIP5 experiment[J]. Geophysical Research Letters,2013-01-01,40(19).
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