Indian summer monsoon variability forecasts in the North American multimodel ensemble

被引:23
|
作者
Singh, Bohar [1 ]
Cash, Ben [2 ]
Kinter, James L., III [2 ]
机构
[1] George Mason Univ, Fairfax, VA 22031 USA
[2] George Mason Univ, Ctr Ocean Land Atmosphere Studies, Fairfax, VA 22031 USA
关键词
Indian Monsoon; Interannual variability; Teleconnections; TO-INTERANNUAL PREDICTION; COUPLED CLIMATE MODELS; SOUTHERN OSCILLATION; GLOBAL PRECIPITATION; EQUATORIAL PACIFIC; TIBETAN PLATEAU; RAINFALL; OCEAN; CIRCULATION; ENSO;
D O I
10.1007/s00382-018-4203-6
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The representation of the seasonal mean and interannual variability of the Indian summer monsoon rainfall (ISMR) in nine global ocean-atmosphere coupled models that participated in the North American Multimodal Ensemble (NMME) phase 1 (NMME:1), and in nine global ocean-atmosphere coupled models participating in the NMME phase 2 (NMME:2) from 1982-2009, is evaluated over the Indo-Pacific domain with May initial conditions. The multi-model ensemble (MME) represents the Indian monsoon rainfall with modest skill and systematic biases. There is no significant improvement in the seasonal forecast skill or interannual variability of ISMR in NMME:2 as compared to NMME:1. The NMME skillfully predicts seasonal mean sea surface temperature (SST) and some of the teleconnections with seasonal mean rainfall. However, the SST-rainfall teleconnections are stronger in the NMME than observed. The NMME is not able to capture the extremes of seasonal mean rainfall and the simulated Indian Ocean-monsoon teleconnections are opposite to what are observed.
引用
收藏
页码:7321 / 7334
页数:14
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