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

Seneviratne, S., Wilhelm, M., Stanelle, T., van den Hurk, B., Hagemann, S., Berg, A., et al. (2013). Impact of soil moisture-climate feedbacks on CMIP5 projections: First results from the GLACE-CMIP5 experiment. Geophysical Research Letters, 40, 5212-5217. doi:10.1002/grl.50956.

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 Creators:
Seneviratne, Sonia., Author
Wilhelm, Micah, Author
Stanelle, Tanja, Author
van den Hurk, Bart, Author
Hagemann, Stefan1, Author           
Berg, Alexis, Author
Cheruy, Frederique, Author
Higgins, Matthew E., Author
Meier, Arndt, Author
Brovkin, Victor2, Author                 
Claussen, Martin3, Author                 
Dufresne, Jean-Louis, Author
Findell, Kirsten, Author
Lawrence, David M., Author
Malyshev, Sergey, Author
Smith, Ben, Author
Affiliations:
1Terrestrial Hydrology, The Land in the Earth System, MPI for Meteorology, Max Planck Society, ou_913560              
2Climate-Biogeosphere Interaction, The Land in the Earth System, MPI for Meteorology, Max Planck Society, ou_913566              
3Director’s Research Group LES, The Land in the Earth System, MPI for Meteorology, Max Planck Society, ou_913564              

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Free keywords: Climate extremes; CMIP5; Feedbacks; Land-atmosphere interactions; Projections; Soil moisture
 Abstract: 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. © 2013.

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Language(s): eng - English
 Dates: 20122013-09-102013-09-102013
 Publication Status: Published in print
 Pages: -
 Publishing info: -
 Table of Contents: -
 Rev. Type: Peer
 Identifiers: DOI: 10.1002/grl.50956
 Degree: -

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Title: Geophysical Research Letters
  Abbreviation : Geophys. Res. Lett.
Source Genre: Journal
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Publ. Info: Washington, D.C. : American Geophysical Union
Pages: - Volume / Issue: 40 Sequence Number: - Start / End Page: 5212 - 5217 Identifier: ISSN: 0094-8276
CoNE: https://pure.mpg.de/cone/journals/resource/954925465217