Impact of soil moisture-climate feedbacks on CMIP5 projections: First results from the GLACE-CMIP5 experiment

被引：294

作者：

Seneviratne, Sonia I. ^{[1
]}

Wilhelm, Micah ^{[1
]}

Stanelle, Tanja ^{[1
]}

van den Hurk, Bart ^{[2
]}

Hagemann, Stefan ^{[3
]}

Berg, Alexis ^{[4
,5
]}

Cheruy, Frederique ^{[6
]}

Higgins, Matthew E. ^{[7
]}

Meier, Arndt ^{[8
]}

Brovkin, Victor ^{[3
]}

Claussen, Martin ^{[3
]}

Ducharne, Agnes ^{[9
]}

Dufresne, Jean-Louis ^{[6
]}

Findell, Kirsten L. ^{[4
]}

Ghattas, Josefine ^{[9
]}

Lawrence, David M. ^{[7
]}

Malyshev, Sergey ^{[10
]}

Rummukainen, Markku ^{[8
]}

Smith, Benjamin ^{[11
]}

机构：

[1] ETH, Inst Atmospher & Climate Sci, CH-8092 Zurich, Switzerland

[2] KNMI, De Bilt, Netherlands

[3] Max Planck Inst Meteorol, D-20146 Hamburg, Germany

[4] NOAA, GFDL, Princeton, NJ USA

[5] Rutgers State Univ, New Brunswick, NJ 08903 USA

[6] Univ Paris 06, LMD IPSL, Paris, France

[7] NCAR, Boulder, CO USA

[8] Lund Univ, Ctr Environm & Climate Res, Lund, Sweden

[9] Univ Paris 06, Lab Sisyphe IPSL, Paris, France

[10] Princeton Univ, Princeton, NJ 08544 USA

[11] Lund Univ, Dept Phys Geog & Ecosyst Sci, Lund, Sweden

来源：

GEOPHYSICAL RESEARCH LETTERS | 2013年 / 40卷 / 19期

基金：

欧盟第七框架计划; 美国国家科学基金会;

关键词：

CMIP5; soil moisture; feedbacks; climate extremes; land-atmosphere interactions; projections; FUTURE CLIMATE; MODEL; LAND; HYDROLOGY; DROUGHT; CYCLE;

D O I：

10.1002/grl.50956

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

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 1-1.5K for mean temperature and 2-2.5K 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.

引用

页码：5212 / 5217

页数：6

共 33 条

[31] ACCELERATION OF LAND SURFACE MODEL DEVELOPMENT OVER A DECADE OF GLASS
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