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基于小时雨量的防城港市短时强降水特征分析
黄春华,黄滢,林文桦,莫权芳,刘金裕
0
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(广西壮族自治区防城港市气象局,广西 防城港 538001)
摘要:
基于2016—2019年防城港市自动气象站小时雨量,结合地形分析短时强降水时空分布特征,结果表明:十万大山南北两侧短时强降水次数从北到南递增,大值区位于十万大山南侧的迎风坡及喇叭口地形;各月的短时强降水的分布有差异,短时强降水主要发生在4—9月,6月短时强降水分布不均匀,7—8月短时强降水最强盛;受对流日变化、低空急流、海陆风等影响,短时强降水日变化特征明显,前汛期市南部短时强降水高峰期出现在清晨、市北部出现在凌晨和午后,后汛期市南部出现在清晨和午后、市北部出现在午后到傍晚,非汛期短时强降水出现的时段呈多峰值态势。
关键词:  短时强降水;地形;时空分布;逐时降水
DOI:
投稿时间:2020-12-11
基金项目:中国气象局预报员专项(CMAYBY2020-099):2019年5月25—28日广西暖区暴雨分析;防城港市气象科研项目(防气科201801号):防城港市强对流天气雷达特征分析
Characteristics of Short-term Intense Rain in Fangchenggang  City Based on Hourly Rainfall Data
HUANG Chunhua,HUANG Ying,LIN Wenhua,MO Quanfang,LIU Jinyu
(Fangchenggang Meteorological Bureau, Fangchenggang 538001 , China)
Abstract:
Based on the hourly rainfall data from automatic weather stations in Fangchenggang from 2016 to2019, the spatial and temporal distribution of short-term intense rain with specific topography is analyzed.The result is shown as follows.The frequency of short-term intense rain increases from north to south across the Shiwandashan; the large-value areas centers in the windward slope on the south side of Shiwandashan and bellmouthed terrain; short-term intense rain mainly occurred from April to September, with an uneven distribution in June and being strongest in July-August; affected by convection diurnal variation, low-level jet stream and sea-land wind, the diurnal variation characteristics are obvious.In general,in the South of Fangchenggang,the peak period of short-term intense rain occurred in the early morning in the first raining season ( April through June),while occurred in early morning and afternoon in the second raining season (July through September);in the North of Fangchenggang,the peak period of short-term intense rain occurred in the early morning and afternoon in the first raining season,while the peak period of short-term intense rain occurred from afternoon to evening in the second raining season; in non-flood season,the period of short-term intense rain presents a multi-peak trend.
Key words:  short-term intense rain; topography; spatiotemporal distribution;hourly rainfall
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