首页|2012~2021年宜昌市强降水时空分布特征

2012~2021年宜昌市强降水时空分布特征

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为深入认识宜昌市强降水时空分布特征,基于 2012~2021 年宜昌市 358 站逐小时降水资料,采用数理统计方法分析该地区1,3,24 h这3 类强降水时空分布和降水极值空间分布特征.结果表明:① 宜昌市 7 个暴雨中心出现在平原向丘陵、山区过渡的迎风坡地带和沿江/河一带,24 h长时累计暴雨南多北少,集中在长江以南,而长江以北地区3h短时暴雨特征明显.②20 mm/h和 30 mm/h以上小时强降水频次分别为 3.8次/a和1.3 次/a,3h短时暴雨、24 h长时累计暴雨频次分别为1.0 次/a和4.9 次/a.小时强降水和3h短时暴雨以2016、2018 年和2020 年最多,24 h长时累计暴雨以2020 年和2016 年发生最为频繁.③3 类强降水频次月变化呈单峰型,主汛期6~8 月为强降水高发期;小时强降水频次日变化呈双峰型,高频次小时强降水集中在13:00 至凌晨04:00,峰值时段为17:00~19:00 和23:00~24:00.④ 宜昌市 3 类降水极值空间分布差异较大,1 h降水量极值和3h降水量极值中东部高于西部,24 h降水量极值中南部高于北部,其高值区主要出现在夷陵区小溪塔街道和乐天溪镇、远安县旧县镇、当阳市河溶镇、宜都市高坝洲镇和聂家河镇、五峰县湾潭镇等地;宜昌市1,3,24 h最大降水量分别为158.8,211.9,363.6 mm.研究成果可为宜昌市强降水预报预警提供参考.
Spatial and temporal distribution of heavy precipitation in Yichang City from 2012 to 2021
To further understand the characteristics of the heavy precipitation in Yichang City,the spatio-temporal distribution of the three types of heavy precipitation,namely 1 h,3 h,and 24 h,and the precipitation extremes were analyzed by using mathe-matical statistics based on hourly precipitation data of 358 meteorological stations in Yichang City from 2012 to 2021.The results showed that:① The seven rainstorm centers in Yichang City usually appeared in the windward slope zone where the plain transits to hills or mountains,and the area along the river.The 24-hour long-duration accumulated rainstorm in the south was more than that in the north,and it was concentrated in the south of the Changjiang River.The 3 h short-duration rainstorm was obvious in the north of the Changjiang River.② The frequency of hourly heavy precipitation above 20 mm/h and 30 mm/h was 3.8 times and 1.3 times per year,respectively.The frequency of 3 h short-duration rainstorms and 24 h long-duration accumulated rain-storms was 1.0 times and 4.9 times per year,respectively.The years of the most frequent hourly heavy precipitation and 3 h short-duration rainstorms were 2016,2018,and 2020.The years of the most frequent 24 h long-duration accumulated rainstorms were 2020 and 2016.③ The monthly variation of three types of heavy precipitation showed an unimodal pattern,with the main flood season from June to August being the peak period for heavy precipitation.The diurnal variation of hourly heavy precipitation showed a bimodal pattern,with the high-frequency hourly heavy precipitation concentrated from 13:00 to 04:00,and peak peri-ods from 17:00 to 19:00 and 23:00 to 24:00.④The spatial distribution of three types of heavy precipitation extremes in Yichang City varied greatly,with 1 h precipitation extremes and 3 h precipitation extremes were higher in the center-east than that in the west,and 24 h precipitation extremes in the center-south were higher than that in the north.Areas with high precipitation ex-tremes mainly appeared in Xiaoxita Street and Letianxi Town in Yiling County,Jiuxian Town in Yuanan County,Herong Town in Dangyang City,Gaobazhou Town and Niejiahe Town in Yidu City,and Wantan Town in Wufeng County.The maximum precipitati-on in Yichang City for 1 h,3 h,and 24 h were 158.8,211.9,and 363.6 mm,respectively.These results can provide references for the classified heavy precipitation forecasting and warning in Yichang City.

heavy precipitationspatio-temporal distributionpeak periodsprecipitation extremesYichang City

刘俊、夏羽、雷东洋、叶丹、枚雪彬、彭福强

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宜昌市气象局,湖北 宜昌 443000

三峡国家气候观象台,湖北 宜昌 443000

武汉中心气象台,湖北 武汉 430074

强降水 时空分布 峰值时段 降水极值 宜昌市

湖北省自然科学基金项目宜昌市气象局自立课题重点项目宜昌市气象局自立课题重点项目

2023AFD106YC202101YCZD202201

2024

人民长江
水利部长江水利委员会

人民长江

CSTPCD北大核心
影响因子:0.451
ISSN:1001-4179
年,卷(期):2024.55(7)
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