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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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Seneviratne, Sonia., Autor
Wilhelm, Micah, Autor
Stanelle, Tanja, Autor
van den Hurk, Bart, Autor
Hagemann, Stefan1, Autor           
Berg, Alexis, Autor
Cheruy, Frederique, Autor
Higgins, Matthew E., Autor
Meier, Arndt, Autor
Brovkin, Victor2, Autor                 
Claussen, Martin3, Autor                 
Dufresne, Jean-Louis, Autor
Findell, Kirsten, Autor
Lawrence, David M., Autor
Malyshev, Sergey, Autor
Smith, Ben, Autor
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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Schlagwörter: Climate extremes; CMIP5; Feedbacks; Land-atmosphere interactions; Projections; Soil moisture
 Zusammenfassung: 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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Sprache(n): eng - English
 Datum: 20122013-09-102013-09-102013
 Publikationsstatus: Erschienen
 Seiten: -
 Ort, Verlag, Ausgabe: -
 Inhaltsverzeichnis: -
 Art der Begutachtung: Expertenbegutachtung
 Identifikatoren: DOI: 10.1002/grl.50956
 Art des Abschluß: -

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Titel: Geophysical Research Letters
  Kurztitel : Geophys. Res. Lett.
Genre der Quelle: Zeitschrift
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Ort, Verlag, Ausgabe: Washington, D.C. : American Geophysical Union
Seiten: - Band / Heft: 40 Artikelnummer: - Start- / Endseite: 5212 - 5217 Identifikator: ISSN: 0094-8276
CoNE: https://pure.mpg.de/cone/journals/resource/954925465217