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Climate Dynamics

, Volume 51, Issue 3, pp 985–1003 | Cite as

Control of radiation and evaporation on temperature variability in a WRF regional climate simulation: comparison with colocated long term ground based observations near Paris

  • S. Bastin
  • M. Chiriaco
  • P. Drobinski
Article

Abstract

The objective of this paper is to understand how large-scale processes, cloud cover and surface fluxes affect the temperature variability over the SIRTA site, near Paris, and in a regional climate simulation performed in the frame of HyMeX/Med-CORDEX programs. This site is located in a climatic transitional area where models usually show strong dispersions despite the significant influence of large scale on interannual variability due to its western location. At seasonal time scale, the temperature is mainly controlled by surface fluxes. In the model, the transition from radiation to soil moisture limited regime occurs earlier than in observations leading to an overestimate of summertime temperature. An overestimate of shortwave radiation (SW), consistent with a lack of low clouds, enhances the soil dryness. A simulation with a wet soil is used to better analyse the relationship between dry soil and clouds but while the wetter soil leads to colder temperature, the cloud cover during daytime is not increased due to the atmospheric stability. At shorter time scales, the control of surface radiation becomes higher. In the simulation, higher temperatures are associated with higher SW. A wet soil mitigates the effect of radiation due to modulation by evaporation. In observations, the variability of clouds and their effect on SW is stronger leading to a nearly constant mean SW when sorted by temperature quantile but a stronger impact of cloud cover on day-to-day temperature variability. Impact of cloud albedo effect on precipitation is also compared.

Keywords

Hymex CORDEX Temperature variability SIRTA-ReOBS Surface and radiative fluxes Lidar simulator Cloud radiative effects Land surface–atmosphere interactions 

Notes

Acknowledgments

This work is a contribution to the HyMeX program (HYdrological cycle in The Mediterranean EXperiment) through INSU-MISTRALS support and the MEDCORDEX program (COordinated Regional climate Downscaling EXperiment—Mediterranean region). This research has received funding from the French National Research Agency (ANR) project REMEMBER (grant ANR-12-SENV-001) and is a contribution to the EECLAT project through LEFE/INSU and TOSCA/CNES supports. It was supported by the IPSL group for regional climate and environmental studies, with granted access to the HPC resources of GENCI/IDRIS (under allocation i2011010227). The SIRTA-ReOBS effort also benefited from the support of the L-IPSL funded by ANR under the “Programme d’Investissements d’Avenir (Grant ANR-10-LABX-0018) and by the EUCLIPSE project funded by the European Commission under the Seventh Framework Program (Grant no 244067). We would like to acknowledge the SIRTA and Climserv teams at IPSL for collecting and providing data and computing ressources; Cindy Lebeaupin-Brossier and Marc Stefanon for providing simulation outputs; the CNES (Centre National d’Etudes Spatiales) for partially funded M. Chiriaco research.

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© Springer-Verlag Berlin Heidelberg 2016

Authors and Affiliations

  1. 1.LATMOS/IPSL, UVSQ Université Paris-Saclay, UPMC Univ. Paris 06CNRSGuyancourtFrance
  2. 2.Laboratoire de Météorologie Dynamique, Ecole Polytechnique, Sorbonne Universités, CNRS/INSUUPMC Univ. Paris 0691128France

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