PRECIPITATION DOWNSCALING UNDER CLIMATE CHANGE: RECENT DEVELOPMENTS TO BRIDGE THE GAP BETWEEN DYNAMICAL MODELS AND THE END USER

被引:1258
作者
Maraun, D. [1 ,2 ]
Wetterhall, F. [3 ]
Ireson, A. M. [4 ]
Chandler, R. E. [5 ]
Kendon, E. J. [6 ]
Widmann, M. [7 ]
Brienen, S. [8 ]
Rust, H. W. [9 ]
Sauter, T. [10 ]
Themessl, M. [11 ]
Venema, V. K. C. [8 ]
Chun, K. P. [4 ]
Goodess, C. M. [2 ]
Jones, R. G. [6 ]
Onof, C. [4 ]
Vrac, M. [9 ]
Thiele-Eich, I. [8 ]
机构
[1] Univ Giessen, Dept Geog, D-35390 Giessen, Germany
[2] Univ E Anglia, Climat Res Unit, Sch Environm Sci, Norwich NR4 7TJ, Norfolk, England
[3] Kings Coll London, Dept Geog, London WC2R 2LS, England
[4] Univ London Imperial Coll Sci Technol & Med, Environm & Water Resources Engn Res Grp, London SW7 2AZ, England
[5] UCL, Dept Stat Sci, London WC1E 6BT, England
[6] Met Off Hadley Ctr, Exeter EX1 3PB, Devon, England
[7] Univ Birmingham, Sch Geog Earth & Environm Sci, Birmingham B15 2TT, W Midlands, England
[8] Univ Bonn, Inst Meteorol, D-53121 Bonn, Germany
[9] Ctr Etud Saclay, CNRS, IPSL, Lab Sci Climat & Environm, F-91191 Gif Sur Yvette, France
[10] Univ Aachen, Rhein Westfal TH Aachen, Dept Geog, D-52056 Aachen, Germany
[11] Graz Univ, Wegener Ctr Climate & Global Change, A-8010 Graz, Austria
关键词
HIDDEN MARKOV MODEL; STOCHASTIC RAINFALL MODEL; REGIONAL-CLIMATE; EXTREME PRECIPITATION; NORTH-ATLANTIC; WEATHER REGIMES; POINT PROCESS; ATMOSPHERIC CIRCULATION; SIMULATED PRECIPITATION; GROUNDWATER RECHARGE;
D O I
10.1029/2009RG000314
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Precipitation downscaling improves the coarse resolution and poor representation of precipitation in global climate models and helps end users to assess the likely hydrological impacts of climate change. This paper integrates perspectives from meteorologists, climatologists, statisticians, and hydrologists to identify generic end user (in particular, impact modeler) needs and to discuss downscaling capabilities and gaps. End users need a reliable representation of precipitation intensities and temporal and spatial variability, as well as physical consistency, independent of region and season. In addition to presenting dynamical downscaling, we review perfect prognosis statistical downscaling, model output statistics, and weather generators, focusing on recent developments to improve the representation of space-time variability. Furthermore, evaluation techniques to assess downscaling skill are presented. Downscaling adds considerable value to projections from global climate models. Remaining gaps are uncertainties arising from sparse data; representation of extreme summer precipitation, subdaily precipitation, and full precipitation fields on fine scales; capturing changes in small-scale processes and their feedback on large scales; and errors inherited from the driving global climate model.
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页数:34
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