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南海夏季风爆发前后低纬大气环流突变特征
引用本文:简茂球,乔云亭,罗会邦.南海夏季风爆发前后低纬大气环流突变特征[J].气候与环境研究,2000,5(4):356-362.
作者姓名:简茂球  乔云亭  罗会邦
作者单位:中山大学大气科学系,广州 510275
基金项目:国家科技部攀登项目A“南海季风试验研究”
摘    要:利用1982~1996年15年平均的NCEP再分析资料,研究南海夏季风爆发前后低纬大气环流的突变特征。结果表明,东南亚地区对流层中上层厚度(温度)场、高低风场和大气层顶净辐射加热率(QRT)都有突变发生。海温场的变化相对其他要素较为缓慢,但也存在明显的转折点。QRT突变最早,其次是海温场变化出现明显转折,再是厚度(温度)场、低层风场突变,高层风场的突变最迟;低层风场突变最快,其次是厚度(温度)场,最后是QRT和高层风场。南海地区的降水,水汽场的突变发生在南海夏季风爆发前,而且突变较快。

关 键 词:南海夏季风  爆发  低纬大气环流  突变
修稿时间:2000年9月1日

The Abrupt Change of the Circulation in Low-Latitudes During the Period From April to June
Jian Maoqiu,Qiao Yunting and Luo Huibang.The Abrupt Change of the Circulation in Low-Latitudes During the Period From April to June[J].Climatic and Environmental Research,2000,5(4):356-362.
Authors:Jian Maoqiu  Qiao Yunting and Luo Huibang
Abstract:The abrupt change of the general circulation over the South China Sea (SCS) and surrounding areas during the period from April to June is studied by using the 15-year mean NCEP daily data of 1982~1996. The significant abrupt change exits in the thickness (averaged temperature) between 500 and 200 hPa levels, the wind at 850 and 200 hPa, and the net radiative heating (QRT) at the top of the atmosphere. The sea surface temperature (SST) evolves more slowly than other variables mentioned above but with a turning point around early May. The abrupt changes in QRT occur around mid-April and at the end of April. Around mid-May occur the abrupt changes simultaneously in the thickness of 500~200 hPa and the wind field at 850 hPa, then followed by the high-level wind. The abrupt changes in the precipitation and the specific humidity over SCS come quite fast and early before the onset of the SCS monsoon.
Keywords:summer monsoon over South China Sea  onset  circulation  abrupt change
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