Future change of temperature and precipitation extremes in South America as derived from the PRECIS regional climate modeling system

被引:281
作者
Marengo, J. A. [1 ]
Jones, R. [2 ]
Alves, L. M. [1 ]
Valverde, M. C. [1 ]
机构
[1] CPTEC INPE, BR-12630000 Sao Paulo, Brazil
[2] Univ Reading, UK Met Off Hadley Ctr, Reading Unit, Reading RG6 6BB, Berks, England
关键词
downscaling; climate change; vulnerability; OBSERVED TRENDS; SIMULATION; SCENARIO; SENSITIVITY; RAINFALL; INDEXES; CHINA;
D O I
10.1002/joc.1863
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Using the PRECIS regional climate modeling system this study analyses the distribution of extremes of temperature and precipitation ill South America in the recent past (1961 - 1990) and in a future (2071 - 2100) climate under the IPCC SRES A2 and B2 emissions scenarios. The results show that for the present climate the model simulates well the spatial distribution of extreme temperature and rainfall events when compared with observations, with temperature the more realistic. The observations over the region are far from comprehensive which compromises the assessment of model quality. In all the future climate scenarios considered all parts of the region would experience significant and often different changes in rainfall and temperature extremes. Ill the future, the occurrence of warm nights is projected to be more frequent in the entire tropical South America while the Occurrence of cold night events is likely to decrease. Significant changes in rainfall extremes and dry spells are also projected. These include increased intensity of extreme precipitation events over most Of Southeastern South America and western Amazonia consistent with projected increasing trends in total rainfall ill these regions. In Northeast Brazil and eastern Amazonia smaller or no changes are seen in projected rainfall intensity though significant changes are seen in the frequency of consecutive dry clays. Copyright (C) 2009 Royal Meteorological Society
引用
收藏
页码:2241 / 2255
页数:15
相关论文
共 72 条
[11]   Towards quantifying uncertainty in transient climate change [J].
Collins, Matthew ;
Booth, Ben B. B. ;
Harris, Glen R. ;
Murphy, James M. ;
Sexton, David M. H. ;
Webb, Mark J. .
CLIMATE DYNAMICS, 2006, 27 (2-3) :127-147
[12]   Acceleration of global warming due to carbon-cycle feedbacks in a coupled climate model [J].
Cox, PM ;
Betts, RA ;
Jones, CD ;
Spall, SA ;
Totterdell, IJ .
NATURE, 2000, 408 (6809) :184-187
[13]   On the role of climate scenarios for adaptation planning [J].
Dessai, S ;
Lu, XF ;
Risbey, JS .
GLOBAL ENVIRONMENTAL CHANGE-HUMAN AND POLICY DIMENSIONS, 2005, 15 (02) :87-97
[14]   Future change of precipitation extremes in Europe:: Intercomparison of scenarios from regional climate models [J].
Frei, C ;
Schöll, R ;
Fukutome, S ;
Schmidli, J ;
Vidale, PL .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2006, 111 (D6)
[15]   Observed coherent changes in climatic extremes during the second half of the twentieth century [J].
Frich, P ;
Alexander, LV ;
Della-Marta, P ;
Gleason, B ;
Haylock, M ;
Tank, AMGK ;
Peterson, T .
CLIMATE RESEARCH, 2002, 19 (03) :193-212
[16]   Projected changes in mean and extreme precipitation over the Mediterranean region from a high resolution double nested RCM simulation [J].
Gao, XJ ;
Pal, JS ;
Giorgi, F .
GEOPHYSICAL RESEARCH LETTERS, 2006, 33 (03)
[17]   Mean, interannual variability and trends in a regional climate change experiment over Europe. I. Present-day climate (1961-1990) [J].
Giorgi, F ;
Bi, X ;
Pal, JS .
CLIMATE DYNAMICS, 2004, 22 (6-7) :733-756
[18]  
Giorgi F, 2001, CLIMATE CHANGE 2001: THE SCIENTIFIC BASIS, P583
[19]   The simulation of SST, sea ice extents and ocean heat transports in a version of the Hadley Centre coupled model without flux adjustments [J].
Gordon, C ;
Cooper, C ;
Senior, CA ;
Banks, H ;
Gregory, JM ;
Johns, TC ;
Mitchell, JFB ;
Wood, RA .
CLIMATE DYNAMICS, 2000, 16 (2-3) :147-168
[20]   Trends in intense precipitation in the climate record [J].
Groisman, PY ;
Knight, RW ;
Easterling, DR ;
Karl, TR ;
Hegerl, GC ;
Razuvaev, VAN .
JOURNAL OF CLIMATE, 2005, 18 (09) :1326-1350