High-resolution projection of climate change and extremity over Israel using COSMO-CLM

被引:50
作者
Hochman, Assaf [1 ,2 ,3 ]
Mercogliano, Paola [4 ,5 ]
Alpert, Pinhas [1 ]
Saaroni, Hadas [3 ]
Bucchignani, Edoardo [4 ,5 ]
机构
[1] Tel Aviv Univ, Sch Geosci, Dept Geosci, IL-69978 Tel Aviv, Israel
[2] Tel Aviv Univ, Porter Sch Environm Studies, Sch Geosci, Tel Aviv, Israel
[3] Tel Aviv Univ, Dept Geog & Human Environm, Sch Geosci, Tel Aviv, Israel
[4] CMCC Euromediterranean Ctr Climate Change, Capua, Italy
[5] CIRA Centro Italiano Ric Aerospaziali, Capua, Italy
关键词
COSMO-CLM; downscaling; eastern Mediterranean; ETCCDI; extreme precipitation; extreme temperature; Israel; RCM; NORTH-AFRICA DOMAIN; PRECIPITATION EVENTS; MIDDLE-EAST; SIMULATIONS; TEMPERATURE; RAINFALL; MOISTURE; TRENDS;
D O I
10.1002/joc.5714
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
High-resolution climate projections over Israel (about 8 km) have been obtained with the regional model COSMO-CLM, nested into the CORDEX-MENA simulations at 25 km resolution. This simulation provides high-resolution spatial variability of total precipitation and precipitation intensity. Projections are presented not only in terms of average properties, but also using a subset of extreme temperature and precipitation indices from the standard Expert Team on Climate Change Detection and Indices (ETCCDI) for the period 2041-2070 with respect to 1981-2010 (RCP4.5). A general increase in seasonal mean temperature is projected throughout the domain with peaks of similar to 2.5 degrees C, especially in winter and autumn. Extreme temperature indices show increases, larger in the minimum than in the maximum temperatures. Regarding total seasonal precipitation, decreases were found in the north and central Mediterranean climate parts of Israel, with reductions reaching similar to 40%, and increases of the same percentage in the most southern arid parts during winter and spring. An increase in precipitation intensity is shown mostly for the southern arid part of the region, with some indications of extremity also in the north. This spatial pattern probably results from a decrease in cyclones' occurrences, which mainly influences the northern and central parts of Israel, and an increase in convective activity in the south. The outcome of this study can serve as a basis for priority setting and policy formulation towards better climate adaptation.
引用
收藏
页码:5095 / 5106
页数:12
相关论文
共 71 条
[1]   Climatic trends to extremes employing regional modeling and statistical interpretation over the E. Mediterranean [J].
Alpert, P. ;
Krichak, S. O. ;
Shafir, H. ;
Haim, D. ;
Osetinsky, I. .
GLOBAL AND PLANETARY CHANGE, 2008, 63 (2-3) :163-170
[2]   The paradoxical increase of Mediterranean extreme daily rainfall in spite of decrease in total values [J].
Alpert, P ;
Ben-Gai, T ;
Baharad, A ;
Benjamini, Y ;
Yekutieli, D ;
Colacino, M ;
Diodato, L ;
Ramis, C ;
Homar, V ;
Romero, R ;
Michaelides, S ;
Manes, A .
GEOPHYSICAL RESEARCH LETTERS, 2002, 29 (11) :31-1
[3]  
ALPERT P, 1986, MON WEATHER REV, V114, P1411, DOI 10.1175/1520-0493(1986)114<1411:AEWPAM>2.0.CO
[4]  
2
[5]  
Alpert P, 2006, CLIVAR EXCHANGES, V11, P12
[6]  
Alpert P., 2005, ADV GEOSCIENCES, V2, P157, DOI [10.5194/adgeo-2-157-2005, DOI 10.5194/ADGEO-2-157-2005]
[7]  
[Anonymous], 2007, Adv Geosci, DOI DOI 10.5194/ADGEO-12-165-2008
[8]   Operational Convective-Scale Numerical Weather Prediction with the COSMO Model: Description and Sensitivities [J].
Baldauf, Michael ;
Seifert, Axel ;
Foerstner, Jochen ;
Majewski, Detlev ;
Raschendorfer, Matthias ;
Reinhardt, Thorsten .
MONTHLY WEATHER REVIEW, 2011, 139 (12) :3887-3905
[9]   Temporal and spatial trends of temperature patterns in Israel [J].
Ben-Gai, T ;
Bitan, A ;
Manes, A ;
Alpert, P ;
Rubin, S .
THEORETICAL AND APPLIED CLIMATOLOGY, 1999, 64 (3-4) :163-177
[10]   Downscaled simulations of the ECHAM5, CCSM3 and HadCM3 global models for the eastern Mediterranean-Black Sea region: evaluation of the reference period [J].
Bozkurt, Deniz ;
Turuncoglu, Ufuk ;
Sen, Omer Lutfi ;
Onol, Baris ;
Dalfes, H. Nuzhet .
CLIMATE DYNAMICS, 2012, 39 (1-2) :207-225