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干旱区地理 ›› 2015, Vol. 38 ›› Issue (5): 912-919.

• 气候与水文 • 上一篇    下一篇

西安市高温闷热天气的气候特征及其环流形势

高红燕1,2, 王丹1, 卢珊1, 杨艳超1, 张宏芳1, 杨新1   

  1. 1. 陕西省气象服务中心, 陕西西安 710014;
    2. 中国气象局兰州干旱气象研究所, 甘肃兰州 730020
  • 收稿日期:2014-12-17 修回日期:2015-03-09 出版日期:2015-09-25
  • 作者简介:高红燕(1966-)女,陕西延川人,学士,高级工程师,主要从事应用气象研究.Email:gaohongyan121@163.com
  • 基金资助:

    陕西省气象局科技创新基金计划项目(2013M-35);中国气象局兰州干旱气象研究所干旱气象科学研究基金项目(zam201306)

Climatologic characteristics and circulation situation of hot day and weltering weather at Xi'an City

GAO Hong-yan1,2, WANG Dan1, LU Shan1, YANG Yan-chao1, ZHANG Hong-fang1, YANG Xin1   

  1. 1. Shaanxi Province Meteorological Service Center, Xi'an 710014;
    2. Lanzhou Institute of Arid Meteorology, The China Meteorological Administration, Gansu, Lanzhou 730020, Gansu, China
  • Received:2014-12-17 Revised:2015-03-09 Online:2015-09-25

摘要: 利用西安市1951-2013年63 a的日最高气温(Tmax ≥ 35℃)资料,对高温日数的月、季、年际、年代际变化特征进行了分析,计算了1980-2013年闷热指数(THI),在此基础上定义了酷热日,比较了高温日数及酷热日数的变化特征和相互联系。结果表明:高温天气具有明显的年代际变化, 20世纪50、60年代高温日数较多,分别为24.7 d·a-1, 26.5 d·a-1, 70年代开始逐渐减少为21.8 d·a-1, 80年代进入低谷期14.5 d·a-1, 90年代开始增多为23.3 d·a-1, 21世纪(2001-2013年)达到最多27.5 d·a-1;高温天气出现的开始日期具有提前趋势,结束日期具有推后的趋势。酷热天气出现的频率明显少于高温天气出现的频率,高温天气出现在4~9月,酷热天气出现在6~9月,而高温酷热出现最多的月份是7月。当酷热日天气出现时, 87.5%的酷热日与高温日相对应,最高气温在32.4℃以上,相对湿度比较大。通过对高温及酷热天气的前10个个例环流形势的分析发现,酷热天气除与高温有关外还与副热带高压的西伸北抬带来的暖湿气流有关,中高层为下沉气流,低层为暖湿气流,形成高温高湿的闷热天气,而单纯的高温天气多与大陆高压或青藏高压的控制密切有关,以深厚的干暖下沉气流为主,天气以晴朗干燥天气为主。

关键词: 高温, 闷热, 对比分析, 环流形势

Abstract: To understanding the climatologic characteristics of hot days and weltering weather at Xi'an City, Shaanxi Province, China during recent decades, the paper analyzed the characteristics of monthly, seasonal, interannual and interdecadal changes of daily maximum temperature using the data of daily maximum temperature in Xi'an station from 1951 to 2013,, and the temperature-humidity index(THI)were calculated with the data of daily maximum temperature and daily minimum relative humid from 1980 to 2013, and an extremely hot day was defined as a day of THI more than 29.5 at the highest five level. With the comparison of hot day with extremely temperature-humidity, the results showed that there was a significant interdecadal variation of hot days, and there had about 24.7 d·a-1 in 1950s and 26.5 d·a-1 in 1960s, but in 1970s, the hot days was reduced to 21.8 d·a-1 and 14.5 d·a-1 in 1980s. In 1990s, the hot days were increased to 23.3 d·a-1, and the number of hot days(27.5 d·a-1) were at most from 2001 to 2013, and that the starting date of hot days was shifted forward and end date was delayed. The number of extremely hot days was significant less than that of hot days, and there were most extremely hot days in the July of a year, and that 87.5% of extremely hot days was related to hot days, which was with above 32.4℃ and high humid. Finally, the relationship between the extremely hot days and atmospheric circulation was studied. The result pointed out that the extremely hot days was significantly related to warm and humid current resulted from the westward and northward of subtropical high, and there was a sinking airflow in middle and high layer, and warm and humid current, hence there was a high humid and hot weather situation, a pure high temperature weather was related to continental high pressure and Tibet plateau high with warm downward flow, and which was dry and clear.

Key words: hot day, weltering weather, comparative analysis, Circulation situation

中图分类号: 

  • P463.1