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Simulating the effect of anthropogenic vegetation land cover on heatwave temperatures over central France

2014; Inter-Research Science Center; Volume: 60; Issue: 2 Linguagem: Inglês

10.3354/cr01230

1616-1572

Marc Stéfanon, Solveig Schindler, Philippe Drobinski, Nathalie de Noblet‐Ducoudré, Fabio D’Andrea,

Fire effects on ecosystems

CR Climate Research Contact the journal Facebook Twitter RSS Mailing List Subscribe to our mailing list via Mailchimp HomeLatest VolumeAbout the JournalEditorsSpecials CR 60:133-146 (2014) - DOI: https://doi.org/10.3354/cr01230 Simulating the effect of anthropogenic vegetation land cover on heatwave temperatures over central France M. Stéfanon1,*, S. Schindler2, P. Drobinski2, N. de Noblet-Ducoudré3, F. D'Andrea2 1Laboratoire d'Écologie Systématique et Évolution (ESE), CNRS/UPSUD/AgroParisTech, Orsay, France 2Laboratoire de Météorologie Dynamique (LMD) - Institut Pierre Simon Laplace, CNRS/Ecole Polytechnique/ENS/UPMC, Paris, France 3Laboratoire des Sciences du Climat et de l'Environnement (LSCE) - Institut Pierre Simon Laplace, CEA/CNRS/UVSQ, Gif sur Yvette, France *Corresponding author: marc.stefanon@u-psud.fr ABSTRACT: Events similar to the 2003 heatwaves in France are likely to become more frequent, more intense and longer by the end of the 21st century. Policies for climate mitigation focus on carbon sequestration techniques while land cover change (LCC) may be a better short-term alternative at regional level. However, LCC impact studies conducted so far have often given contradictory results at mid-latitudes for summer temperature. Using a regional climate model, the impact of an afforestation scenario is evaluated for the years 2002 and 2003, and compared to an agricultural scenario. The favorable meteorological conditions in spring 2003 promote the development of agricultural vegetation compared to (1) conditions in 2002 and (2) tree phenology in the forested scenario. This dampens the extreme values of temperature from April to the end of June 2003 (up to 3°C during the June heatwave). From early July to October, drought conditions cause crop failure, while forests are not affected by the lack of soil moisture owing to a deeper root system. Evapotranspiration is therefore smaller in the agricultural scenario, thus amplifying the July-August extreme temperatures. However this cooling capacity of trees in the afforestation scenario is limited during the August heatwave because the high temperatures reach a critical level above which the stomata close and transpiration is inhibited. Our experimental set-up highlights the role of climate-vegetation interactions during extreme events and demonstrates how choices of vegetation cover (e.g. trees versus crops) may substantially modify the summer temperatures in mid-latitude regions. KEY WORDS: Heatwave · Vegetation · Land cover change · Phenology · Regional climate model · Afforestation Full text in pdf format PreviousNextCite this article as: Stéfanon M, Schindler S, Drobinski P, de Noblet-Ducoudré N, D'Andrea F (2014) Simulating the effect of anthropogenic vegetation land cover on heatwave temperatures over central France. Clim Res 60:133-146. https://doi.org/10.3354/cr01230 Export citation RSS - Facebook - Tweet - linkedIn Cited by Published in CR Vol. 60, No. 2. Online publication date: June 17, 2014 Print ISSN: 0936-577X; Online ISSN: 1616-1572 Copyright © 2014 Inter-Research.