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冬季太平洋SST异常对风暴轴和急流的影响
引用本文:朱伟军,孙照渤,彭加毅.冬季太平洋SST异常对风暴轴和急流的影响[J].南京气象学院学报,1999,22(4):575-581.
作者姓名:朱伟军  孙照渤  彭加毅
作者单位:南京气象学院大气科学系,南京,210044
基金项目:国家自然科学基金!49475258
摘    要:利用观测资料分析了冬季太平洋表温度异常对风暴轴和急流的影响。结果表明:在冬季黑潮区域正SST异常进,风暴轴和急流均明显北移,并且风暴辆的强度在入口区显著增强,急流核的中心强度却变化不大;而在冬季赤道中,东太平洋地区正SST异常时,风暴轴和急流主要向东南方向明显扩展,强度也在太平洋中东部显著增强,但急流核的中心强度同样变化不大。

关 键 词:风暴轴  急流  海表温度异常  斜压性
修稿时间:1999-03-10

EFFECTS OF WINTER PACIFIC SSTA ON THE STORM TRACK AND JET STREAM
Zhu Weijun,Sun Zhaobo,Peng Jiayi.EFFECTS OF WINTER PACIFIC SSTA ON THE STORM TRACK AND JET STREAM[J].Journal of Nanjing Institute of Meteorology,1999,22(4):575-581.
Authors:Zhu Weijun  Sun Zhaobo  Peng Jiayi
Abstract:Observational analysis is conducted of the effects of winter Pacific SSTA on the storm track and jet stream.It is shown that the positive Kuroshio (equatorial central and eastern Pacific) SSTA in winter can give rise to northward (east and south ward) movement of both the storm track and jet stream, and lead to substantial enhancement in the entrance aera of the storm track (central and eastern Pacific), but leave the center of jet stream little variation in intensity.As such, the jet stream varies in position and intensity mainly as a result of the change of temperature gradient in the tropics and subtropics,while the variation of the storm track in position and intensity is not only related to the jet stream,but also to the intensified baroclinicity which is mainly caused by diabatic heating.
Keywords:storm track  jet stream  SSTA  baroclinicity
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