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2010年1月广西冬季暴雨水汽特征分析

黄翠银

气象研究与应用2011,Vol.32Issue(4):20-22,48,4.
气象研究与应用2011,Vol.32Issue(4):20-22,48,4.

2010年1月广西冬季暴雨水汽特征分析

Analysis on the Water Vapor Characteristics of Winter Torrential Rain in Jan. 2010 of Guangxi

黄翠银1

作者信息

  • 1. 南宁市气象局,广西南宁530022
  • 折叠

摘要

Abstract

Based on the regular data and NCEP 1×1° from the torrential rain process, which last two days over Guangxi, the convergence, saturation level and sources of water vapor were analyzed to find out the water vapor characteristics of this winter torrential rain. The results show that the water vapor convergence is mainly less than 600 hPa, the strongest moisture convergence is near 850 hPa; the rising motion above Guangxi is severe during the heavy rainfall. The increased flow will carry low water vapor aloft and the water vapor saturation layer over Guangxi reach as high as 200 hPa during the heavy rain. Water vapor required by heavy rainfall comes from west Pacific.

关键词

冬季/暴雨/水汽特征

Key words

winter/torrential rain/characteristics of vapor

分类

天文与地球科学

引用本文复制引用

黄翠银..2010年1月广西冬季暴雨水汽特征分析[J].气象研究与应用,2011,32(4):20-22,48,4.

气象研究与应用

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