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Improved confidence in climate change projections of precipitation further evaluated using daily statistics from ENSEMBLES models
被引:96
|作者:
Boberg, Fredrik
[1
]
Berg, Peter
[2
,3
]
Thejll, Peter
[1
]
Gutowski, William J.
[4
]
Christensen, Jens H.
[1
]
机构:
[1] Danish Meteorol Inst, Danish Climate Ctr, DK-2100 Copenhagen O, Denmark
[2] Univ Karlsruhe, Inst Meteorol & Climate Res, D-76344 Eggenstein Leopoldshafen, Germany
[3] Forschungszentrum Karlsruhe, D-76344 Eggenstein Leopoldshafen, Germany
[4] Iowa State Univ, Dept Geol & Atmospher Sci, Ames, IA 50011 USA
基金:
美国国家科学基金会;
关键词:
Precipitation;
Probability density function;
Regional climate models;
Climate change;
Extreme events;
EUROPEAN CLIMATE;
WATER-BUDGET;
TEMPERATURE;
EXTREMES;
TRENDS;
SIMULATIONS;
AUSTRALIA;
EVENTS;
RAIN;
D O I:
10.1007/s00382-009-0683-8
中图分类号:
P4 [大气科学(气象学)];
学科分类号:
0706 ;
070601 ;
摘要:
Probability density functions for daily precipitation data are used as a validation tool comparing station measurements to seven transient regional climate model runs, with a horizontal resolution of 25 km and driven by the SRES A1B scenario forcing, within the ENSEMBLES project. The validation is performed for the control period 1961-1990 for eight predefined European subregions, and a ninth region enclosing all eight subregions, with different climate characteristics. Models that best match the observations are then used for making climate change projections of precipitation distributions during the twenty-first century for each subregion separately. We find, compared to the control period, a distinct decrease in the contribution to the total precipitation for days with moderate precipitation and a distinct increase for days with more intense precipitation. This change in contribution to the total precipitation is found to amplify with time during all of the twenty-first century with an average rate of 1.1% K-1. Furthermore, the crossover point separating the decreasing from the increasing contributions does not show any significant change with time for any specific subregion. These results are a confirmation and a specification of the results from a previous study using the same station measurements but with a regional climate model ensemble within the PRUDENCE project.
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页码:1509 / 1520
页数:12
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