Impact of soil moisture‐climate feedbacks on CMIP5 projections: First results from the GLACE‐CMIP5 experiment
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- Sonia I. Seneviratne
- Institute for Atmospheric and Climate Science ETH Zurich Zurich Switzerland
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- Micah Wilhelm
- Institute for Atmospheric and Climate Science ETH Zurich Zurich Switzerland
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- Tanja Stanelle
- Institute for Atmospheric and Climate Science ETH Zurich Zurich Switzerland
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- Bart van den Hurk
- KNMI De Bilt Netherlands
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- Stefan Hagemann
- Max Planck Institute for Meteorology Hamburg Germany
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- Alexis Berg
- GFDL, NOAA Princeton New Jersey USA
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- Frederique Cheruy
- LMD/IPSL Université Pierre et Marie Curie Paris France
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- Matthew E. Higgins
- NCAR Boulder Colorado USA
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- Arndt Meier
- Centre for Environmental and Climate Research Lund University Lund Sweden
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- Victor Brovkin
- Max Planck Institute for Meteorology Hamburg Germany
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- Martin Claussen
- Max Planck Institute for Meteorology Hamburg Germany
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- Agnès Ducharne
- Laboratoire Sisyphe/IPSL Université Pierre et Marie Curie Paris France
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- Jean‐Louis Dufresne
- LMD/IPSL Université Pierre et Marie Curie Paris France
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- Kirsten L. Findell
- GFDL, NOAA Princeton New Jersey USA
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- Joséfine Ghattas
- Laboratoire Sisyphe/IPSL Université Pierre et Marie Curie Paris France
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- David M. Lawrence
- NCAR Boulder Colorado USA
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- Sergey Malyshev
- Princeton University Princeton New Jersey USA
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- Markku Rummukainen
- Centre for Environmental and Climate Research Lund University Lund Sweden
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- Benjamin Smith
- Department of Physical Geography and Ecosystem Science Lund University Lund Sweden
書誌事項
- 公開日
- 2013-10
- 権利情報
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- http://creativecommons.org/licenses/by-nc-nd/3.0/
- DOI
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- 10.1002/grl.50956
- 公開者
- American Geophysical Union (AGU)
この論文をさがす
説明
<jats:title>Abstract</jats:title><jats:p>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.</jats:p>
収録刊行物
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- Geophysical Research Letters
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Geophysical Research Letters 40 (19), 5212-5217, 2013-10
American Geophysical Union (AGU)