###
气象:2009,35(12):37-43
本文二维码信息
码上扫一扫!
2000年以来江淮梅雨带北移的可能成因分析
(1.广东省气候中心, 广州 510080;2.中国气象局广州热带海洋气象研究所;3.中国气象局国家气候中心)
Possible Reasons for Northward Shift of Meiyu Belt in Yangtze Huaihe River Region During 2000-2005
(1.Guangdong Climate Center, Guangzhou 510080;2.Institute of Tropical and Marin e Meteorology, China Meteorological Administration (CMA);3.National Climate Center)
摘要
图/表
参考文献
相似文献
本文已被:浏览 1730次   下载 2639
投稿时间:2008-09-27    修订日期:2009-09-10
中文摘要: 2000年以来长江中下游地区梅雨量偏少年出现的频率大大增加,梅雨量进入一个相对偏少的 时期。观测资料分析表明,2000—2005年江淮梅雨带的位置较1971—1999年向北移动了2个 纬距,淮河流域降水增加了20%。采用1971—2005年NCEP/NCAR再分析资料,从高层风场、中 层位势高度场、低层相对涡度、垂直速度、整层视热源Q1和视水汽汇Q2等角度分析了近6年 大气环流的异常,进一步研究得到:西太平洋副热带高压脊位置的北移、东亚夏季风的加强 以及冷空气的减弱,可能是导致2000—2005年梅雨带位置北移的原因。
Abstract:Since 2000, the probability of deficit Meiyu year has increased and Meiyu rainfall has stepped into a period of decrease in the Yangtze River regio n. The rainfall observational data show that the axis of Meiyu belt has shifted 2 degrees in latitude northwards and the rainfall has increased by 20% in the Huaihe River region during 2000-2005 in comparison with that of 1971-1999. Therefore, a ccording to the NCEP/NCAR reanalysis data, the anomaly situation of general circulation has been analyzed from the aspects of 200hPa wind field, 500hPa potential height field, 850hPa relative vorticity field, vertical velocity, apparentpparent water vapor sink (Q2) for the recent 6 years. In the end, the research s hows that all of the northward movement of the ridge line location of the West Pacific subtropical high, the reinforcement of the East Asian summer monsoon circulation and the weakening of cold air from the north have contributed to the northward shift of Meiyu belt during 2000-2005 in the Yangtze Huaihe River region.
文章编号:     中图分类号:    文献标志码:
基金项目:国家自然科学基金(40705026)和中国气象局广州区域气象中心气象 科技攻关项目(GRMC2007B01)资助
引用文本:
胡娅敏,丁一汇,2009.2000年以来江淮梅雨带北移的可能成因分析[J].气象,35(12):37-43.
Hu Yamin,Ding Yihui,2009.Possible Reasons for Northward Shift of Meiyu Belt in Yangtze Huaihe River Region During 2000-2005 [J].Meteor Mon,35(12):37-43.