###
气象:1999,25(9):21-23
本文二维码信息
码上扫一扫!
黑潮暖流与洞庭湖区汛期降水和洪涝的关系
(湖南省气象台,长沙 410007)
Interconnection between Kuro shio and the Precipitation over the Dongtinghu Area in Summer
摘要
图/表
参考文献
相似文献
本文已被:浏览 720次   下载 1247
    
中文摘要: 以西北太平洋海温和湖南洞庭湖区汛期降水为基本资料,分析前一年秋冬季黑潮暖流区海温与洞庭湖区汛期降水和洪涝的关系。结果表明,洞庭湖区汛期降水与前一年秋冬季黑潮暖流区海温之间存在着十分显著的遥相关关系,黑潮暖流区海温异常是导致大气环流异常,造成洞庭湖区汛期降水异常和洪涝发生的重要气候背景之一。利用该区域海温变异预测洞庭湖区汛期降水趋势效果较好。
Abstract:Using the ocean temperature of Northwest Pacific and the precipitation in summer of Hunan,the interconnection between Kuro-shio from last autumn to last winter and the precipitation and flood in summer in the Dongtinghu area were analysed.The results show that the interconnection between the Kuro-shio in the period and the precipitation and flood in summer in the Dongtinghu area is very outstanding.The anomaly of Kuro-shio is an important background of climate that influences precipitation anomaly and flood in summer in the Dongtinghu area.
文章编号:     中图分类号:    文献标志码:
基金项目:
Author NameAffiliation
  
引用文本:
余曼平,1999.黑潮暖流与洞庭湖区汛期降水和洪涝的关系[J].气象,25(9):21-23.
,1999.Interconnection between Kuro shio and the Precipitation over the Dongtinghu Area in Summer[J].Meteor Mon,25(9):21-23.