SEASONAL PREDICTIONS FOR SPRING AND AUTUMN SURFACE AIR TEMPERATURES OVER SOUTHERN CHINA BY THE NCEP CFSV2

被引:0
|
作者
李婵珠 [1 ]
杨崧 [1 ,2 ,3 ]
李春晖 [4 ]
刘俊荷 [5 ]
机构
[1] School of Atmospheric Sciences, Sun Yat-sen University
[2] Guangdong Province Key Laboratory for Climate Change and Natural Disaster Studies, Sun Yat-sen University
[3] Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai)
[4] Guangzhou Institute of Tropical and Marine Meteorology/Guangdong Provincial Key Laboratory of Regional Numerical Weather Prediction
[5] Thai Meteorological Department, Bangna
基金
中国国家自然科学基金;
关键词
southern China temperature; NCEP CFSv2; prediction; spring; autumn;
D O I
10.16555/j.1006-8775.2019.04.003
中图分类号
P45 [天气预报];
学科分类号
0706 ; 070601 ;
摘要
In this study, we investigate the variations of spring and autumn air temperatures in southern China(SC) and associated atmospheric circulation patterns. During the boreal spring, the SC air temperature is mainly influenced by tropical sea surface temperature anomalies(SSTAs). On the one hand, the El Ni?o SSTA pattern may induce a stronger-than-normal western Pacific subtropical high, which leads to warming in SC. On the other hand, the warm SSTAs in the tropical Indian Ocean may trigger anomalous Rossby wave trains, which propagate northeastward and result in anomalously high temperature in SC. During the boreal autumn, however, the SC temperature is more likely to be affected by the mid-latitude atmospheric circulation, such as the wave trains forced by the North Atlantic SSTAs.The NCEP Climate Forecast System version 2(CFSv2) is able to capture the climatology of SC air temperatures during both spring and autumn. For interannual variation, the CFSv2 shows a good skill for predicting the SC temperature in spring, due to the model’s good performance in capturing the associated atmospheric circulation anomalies as responses to tropical SSTAs, in spite of the overestimated relationship with the El Ni?o-Southern Oscillation(ENSO). However,the model has a poor skill for predicting the SC temperature in autumn, primarily due to the unrealistic prediction of its relationship with the ENSO.
引用
收藏
页码:448 / 461
页数:14
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