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滑动时间窗长度对太行山区雷达反演降水的影响

高烽 周新尧 孔凡超 杨永辉 郭迎春 孙强

气象2018,Vol.44Issue(4):538-547,10.
气象2018,Vol.44Issue(4):538-547,10.DOI:10.7519/j.issn.1000-0526.2018.04.007

滑动时间窗长度对太行山区雷达反演降水的影响

Impact of Moving Time Window Size on Radar-Based Precipitation Estimation in Taihang Mountains

高烽 1周新尧 2孔凡超 1杨永辉 3郭迎春 1孙强3

作者信息

  • 1. 中国科学院遗传与发育生物学研究所农业资源研究中心/中国科学院农业水资源重点实验室/河北省节水农业重点实验室,石家庄050021
  • 2. 中国科学院大学,北京100049
  • 3. 河北省气象台,石家庄050021
  • 折叠

摘要

Abstract

Precise estimation of precipitation in Taihang Mountains is crucial for understanding water cycle and providing support for water management in Haihe River Basin.By using Doppler radar,this study de-veloped the Z-I relationships with different time windows (1-5h) in three counties in eastern side of Taihang Mountains using radar reflectivity (Z) and rain gauge data (I) from June to September during 2013-2014.By dividing the 45 precipitation events into three categories:Light,moderate and heavy,pre-cipitation was precisely estimated from different Z-I relationships under different categories.Take the rainfall event on 9 July 2013 as an example.It showed that (1) the errors of estimated precipitation from different time windows declined firstly,then rose up as the time windows moved from 1 h to 5 h,and the lowest error appeared in 2 h.(2) The 2 h Z-I relationship greatly improved the precision of moderate rain. (3) The estimation of heavy rain also improved when the 2 h Z-I relationship was applied to the rainfall event that happened on 9 July 2013.

关键词

多普勒雷达/降水反演/Z-I关系/滑动时间窗Z-I算法/太行山区

Key words

Doppler radar/precipitation estimation/Z-I relationship/moving time window method/Taihang Mountains

分类

天文与地球科学

引用本文复制引用

高烽,周新尧,孔凡超,杨永辉,郭迎春,孙强..滑动时间窗长度对太行山区雷达反演降水的影响[J].气象,2018,44(4):538-547,10.

基金项目

国家自然科学基金项目(41671021)和河北省自然科学基金项目(D2015503016)共同资助 (41671021)

气象

OA北大核心CSCDCSTPCD

1000-0526

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