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摘要:
[Objective]The research aimed to analyze ' 96. 8' heavy rainstorm process causing flood disaster in Handan. [Method]Based on actual situation data,satellite cloud data and NCEP reanalysis data in the first dekad of August in 1996,' 96. 8' heavy rainstorm process causing flood disaster in Handan was analyzed to understand occurrence reason of the flood disaster. [Result]Two meso-scale convective cloud clusters which developed and went north in turn caused ' 96. 8' heavy rainstorm in Handan. Typhoon and inverted trough were main weather systems induced flood disaster in Handan. In going north process of the low-level jet,due to blocking of the subtropical high,water vapor and energy accumulated in Handan,providing material basis for formation of the heavy rainstorm. Development and eastward movement of the short-wave trough at middle latitude and continuous invasion of the reflux weak cold air at the low layer were direct reason for triggering generation and development of the convective cloud cluster,and further causing continuous rainstorm. Wet layer over the rainstorm zone was deep and thick. Meridional distribution of the wet zone was wider than latitudinal distribution. South China Sea and Bay of Bengal were water vapor sources for the rainstorm zone. In the whole rainstorm period,it was convergence at low layer and divergence at high layer in the rainstorm zone. It was positive vorticity at low layer and negative vorticity at high layer. Precipitation intensity changed as convergence and divergence. Rainstorm zone had strong ascending motion. As strengthening and uplifting of the ascending motion strong center,strong precipitation also strengthened. Rainstorm center was near the biggest vertical velocity center. Strong precipitation changed as vertical ascending motion. [Conclusion]The research provided scientific basis for disaster prevention and reduction and decision-making service.
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篇名 Analysis on " 96. 8" Heavy Rainstorm Process in Handan
来源期刊 气象与环境研究:英文版 学科 地球科学
关键词 大暴雨过程 邯郸市 中尺度对流云团 NCEP再分析资料 卫星云图资料 上升运动 灾害过程 暴雨洪涝
年,卷(期) 2012,(8) 所属期刊栏目
研究方向 页码范围 18-23
页数 6页 分类号 P458.121.1
字数 语种
DOI
五维指标
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研究主题发展历程
节点文献
大暴雨过程
邯郸市
中尺度对流云团
NCEP再分析资料
卫星云图资料
上升运动
灾害过程
暴雨洪涝
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研究分支
研究去脉
引文网络交叉学科
相关学者/机构
期刊影响力
气象与环境研究:英文版
双月刊
2152-3940
出版文献量(篇)
1887
总下载数(次)
1
总被引数(次)
0
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