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熊明明, 徐姝, 李明财, 杨艳娟, 任雨, 曹经福. 2016: 天津地区小时降水特征分析. 暴雨灾害, 35(1): 84-90. DOI: 10.3969/j.issn.1004-9045.2016.01.012
引用本文: 熊明明, 徐姝, 李明财, 杨艳娟, 任雨, 曹经福. 2016: 天津地区小时降水特征分析. 暴雨灾害, 35(1): 84-90. DOI: 10.3969/j.issn.1004-9045.2016.01.012
XIONG Mingming, XU Shu, LI Mingcai, YANG Yanjuan, REN Yu, CAO Jingfu. 2016: Characteristics of hourly precipitation in Tianjin. Torrential Rain and Disasters, 35(1): 84-90. DOI: 10.3969/j.issn.1004-9045.2016.01.012
Citation: XIONG Mingming, XU Shu, LI Mingcai, YANG Yanjuan, REN Yu, CAO Jingfu. 2016: Characteristics of hourly precipitation in Tianjin. Torrential Rain and Disasters, 35(1): 84-90. DOI: 10.3969/j.issn.1004-9045.2016.01.012

天津地区小时降水特征分析

Characteristics of hourly precipitation in Tianjin

  • 摘要: 利用2009—2013年天津地区205个自动气象站的逐时降水资料, 分析了天津地区降水的基本空间分布和日变化特征。结果表明: (1)天津地区降水小时数及小时平均降水强度空间差异明显, 高值区分别位于蓟县北部山区、市区西北侧、滨海新区中南部; (2)天津中北部地区累积降水量峰值主要出现在23—03时, 南部地区则出现在17—19时和04—08时, 降水频次峰值基本都出现在00—09时, 降水强度峰值与累积降水量峰值出现时间类似, 11时为降水强度低谷出现时间; (3)全市傍晚至午夜的降水频次明显较凌晨偏少, 长持续时间(10 h以上)的最大降水易出现在凌晨至清晨, 短时降水(1~4 h)的最大降水易出现在傍晚至午夜; 13—24时多数时次, 无论降水量、频次还是降水强度市区均较其周边地区和沿海地区偏多偏强, 而凌晨多数时次, 市区则以偏少偏弱为主; (4)始于下午至傍晚的降水多为短时降水, 而始于傍晚至凌晨的降水持续时间普遍较长。

     

    Abstract: Based on the hourly rain-gauge data from 205 automatic weather stations (AWS) in Tianjin area during the period of 2009-2013, the basic precipitation distribution and diurnal variation characteristics were analyzed. The results show that there are several high value areas of precipitation hours and hourly precipitation intensities in Tianjin, located in northern mountainous area of Jixian, northwest of the main urban area and the central and south in Binhai New Area. The peak of cumulative precipitation in central and north of Tianjin mainly appears around 23:00-3:00, while it in south mainly appears around 17:00-19:00 and 4:00-8:00. The hourly precipitation intensities are similar to the cumulative precipitation and the lowest value is at 11:00. The peak of precipitation frequency generally appears around 0:00-9:00. The precipitation frequency in early evening to midnight is less than that in the early morning. The maximum value of long duration precipitation often appears in the early morning to morning, while the short duration precipitation often appears in the early evening to midnight. For most times from evening to midnight, the precipitation, precipitation frequency and precipitation intensity in urban areas are stronger than its surrounding areas and coastal areas. But in the morning opposite is true. In Tianjin, precipitation with onset time from afternoon to the evening commonly is short duration precipitation, while precipitation with onset time from the evening to early morning is often long duration precipitation.

     

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