globalchange  > 过去全球变化的重建
DOI: 10.1007/s00382-012-1558-y
Scopus记录号: 2-s2.0-84878111021
论文题名:
Precipitation and temperature space-time variability and extremes in the Mediterranean region: Evaluation of dynamical and statistical downscaling methods
作者: Flaounas E.; Drobinski P.; Vrac M.; Bastin S.; Lebeaupin-Brossier C.; Stéfanon M.; Borga M.; Calvet J.-C.
刊名: Climate Dynamics
ISSN: 9307575
出版年: 2013
卷: 40, 期:2017-11-12
起始页码: 2687
结束页码: 2705
语种: 英语
英文关键词: Climate extremes ; CORDEX ; Downscaling ; HyMeX ; MED-CORDEX ; Mediterranean climate ; Seasonal variability
英文摘要: This study evaluates how statistical and dynamical downscaling models as well as combined approach perform in retrieving the space-time variability of near-surface temperature and rainfall, as well as their extremes, over the whole Mediterranean region. The dynamical downscaling model used in this study is the Weather Research and Forecasting (WRF) model with varying land-surface models and resolutions (20 and 50 km) and the statistical tool is the Cumulative Distribution Function-transform (CDF-t). To achieve a spatially resolved downscaling over the Mediterranean basin, the European Climate Assessment and Dataset (ECA&D) gridded dataset is used for calibration and evaluation of the downscaling models. In the frame of HyMeX and MED-CORDEX international programs, the downscaling is performed on ERA-I reanalysis over the 1989-2008 period. The results show that despite local calibration, CDF-t produces more accurate spatial variability of near-surface temperature and rainfall with respect to ECA&D than WRF which solves the three-dimensional equation of conservation. This first suggests that at 20-50 km resolutions, these three-dimensional processes only weakly contribute to the local value of temperature and precipitation with respect to local one-dimensional processes. Calibration of CDF-t at each individual grid point is thus sufficient to reproduce accurately the spatial pattern. A second explanation is the use of gridded data such as ECA&D which smoothes in part the horizontal variability after data interpolation and damps the added value of dynamical downscaling. This explains partly the absence of added-value of the 2-stage downscaling approach which combines statistical and dynamical downscaling models. The temporal variability of statistically downscaled temperature and rainfall is finally strongly driven by the temporal variability of its forcing (here ERA-Interim or WRF simulations). CDF-t is thus efficient as a bias correction tool but does not show any added-value regarding the time variability of the downscaled field. Finally, the quality of the reference observation dataset is a key issue. Comparison of CDF-t calibrated with ECA&D dataset and WRF simulations to local measurements from weather stations not assimilated in ECA&D, shows that the temporal variability of the downscaled data with respect to the local observations is closer to the local measurements than to ECA&D data. This highlights the strong added-value of dynamical downscaling which improves the temporal variability of the atmospheric dynamics with regard to the driving model. This article highlights the benefits and inconveniences emerging from the use of both downscaling techniques for climate research. Our goal is to contribute to the discussion on the use of downscaling tools to assess the impact of climate change on regional scales. © 2012 Springer-Verlag Berlin Heidelberg.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/54905
Appears in Collections:过去全球变化的重建

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作者单位: Laboratoire de Météorologie Dynamique, Institut Pierre Simon Laplace, CNRS and Ecole Polytechnique, Palaiseau, France; Laboratoire des Sciences du Climat et de l'Environnement, Institut Pierre Simon Laplace, CNRS and CEA, Saclay, France; Laboratoire Atmosphères, Milieux, Observations Spatiales, Institut Pierre Simon Laplace, CNRS and Ecole Polytechnique, Palaiseau, France; Unité de Mécanique, Ecole Nationale Supérieure des Techniques Avancées-ParisTech, Palaiseau, France; Dipartimento Territorio e Sistemi Agro-Forestali, University of Padova, 35020 Legnaro PD, Italy; CNRM/GAME, Météo-France and CNRS, Toulouse, France

Recommended Citation:
Flaounas E.,Drobinski P.,Vrac M.,et al. Precipitation and temperature space-time variability and extremes in the Mediterranean region: Evaluation of dynamical and statistical downscaling methods[J]. Climate Dynamics,2013-01-01,40(2017-11-12)
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