水文与气候变化

近50年山西高温日的时空分布及环流特征

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  • 1. 山西省气象台,太原030006;
    2. 山西省气象局,太原030002;
    3. 山西省气象科技服务中心,太原030002;
    4. 山西省气象局培训中心,太原030012
苗爱梅(1960-),女,山西长治人,正研级高工,主要研究方向为天气、气候与气候变化。E-mail: mam1226@163.com

收稿日期: 2011-01-01

  修回日期: 2011-04-01

  网络出版日期: 2011-07-25

基金资助

山西省科技攻关项目(20090311083)。

The Temporal and Spatial Distributions and Circulation Features of High Temperature Days during last 50 years in Shanxi

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  • 1. Shanxi Meteorological Observatory, Taiyuan 030006, China;
    2. Shanxi Meteorological Bureau, Taiyuan 030002, China;
    3. Shanxi Meteorological Scientific and Technological Service Center, Taiyuan 030002, China;
    4. Shanxi Meteorological Training Center,Taiyuan 030012, China

Received date: 2011-01-01

  Revised date: 2011-04-01

  Online published: 2011-07-25

摘要

利用1958-2008 年高低空气象观测资料以及山西省气象信息中心归档的109 站原始气象记录月报表及其信息化产品资料,分别以最高气温≥35℃、≥37℃、≥40℃为指标, 研究山西高温日的时空分布、变化趋势及环流特征,结果表明:①山西高温日最早出现在4 月中旬,最晚出现在9 月中旬,≥35℃、≥37℃和≥40℃的高温日均是6月下旬最多。②高温日数具有随纬度、随海拔的升高而减少,西部多于东部、南部多于北部、盆地多于山区的空间分布特征。≥40℃的高温区域主要集中在运城和临汾地区。③1984-2008 年,35℃以上的高温日数整体呈上升趋势;1979-2008 年,30a 间高温站次以153 站次/10a 的趋势增多;进入90 年代以后,不仅高温日数增多,而且高温持续时间、强度、范围都有增强趋势。④影响山西高温的500 hPa 环流形势主要有:副高纬向性、副高经向型以及大陆高压(脊)控制型3 类。在特定的流型配置下,T850≥25℃、T700≥13℃,T850≥26℃、T700≥14℃,T850≥28℃、T700≥15℃,T850≥32℃、T700≥16℃是山西省不同区域、不同风向影响时,≥35℃、≥37℃、≥40℃高温天气预报的临界值。

本文引用格式

苗爱梅, 贾利冬, 李苗, 范光海 . 近50年山西高温日的时空分布及环流特征[J]. 地理科学进展, 2011 , 30(7) : 837 -845 . DOI: 10.11820/dlkxjz.2011.07.008

Abstract

With the high-low air meteorological observational data, the original meteorological record, monthly report and meteorological information of 109 stations during 1958-2008 archived by Shanxi Meteorological Information Center, taking the highest temperatures of ≥35℃, ≥37℃ and ≥40℃ as indexes, this paper studies the temporal and spatial distributions, changing trend and circulation features of high temperature days in Shanxi. The results are shown as follows. (1) The earliest high temperature day appears in mid-April in Shanxi, and the latest appears in mid- September, the days with high temperatures of ≥35℃, ≥37℃ and ≥40℃ are in late June. (2) The high temperature days decrease with the increase of latitude and sea level elevation. The areas with high temperatures of ≥40℃ are mostly centralized in Yuncheng and Linfen. (3) The high temperature days of ≥35℃ show a rising trend during 1984-2008. During the 31-year period from 1979 to 2008, the high temperature station frequencies are increased 153 times per 10a. After entering the 1990s, not only the high temperature days, but also the duration, strength, range of the high temperature are increased. (4) There are three types of 500 hPa circulation patterns which can influence Shanxi high temperature: zonal type of the horse latitude high, meridional type of the horse latitude high, and controlling type of continental pressure ridge. Under some special flow pattern configurations, T850≥25℃, T700≥13℃, T850≥26℃, T700≥14℃, T850≥28℃, T700≥15℃, T850≥32℃ and T700≥16℃ are critical values for ≥35℃, ≥37℃ and ≥40℃ high temperature weather forecasts under the influence of wind directions in different regions in Shanxi.

参考文献

[1] Karl T R, Kukla G, Razuvayev V N, et al. Global Warming: Evidence for asymmetric diurnal temperature change. Geophysical Research Letters, 1991, 18(10): 2253 -2256.

[2] Horton B. Geographical distribution of changes in maximum and minimum temperatures. Atmospheric Research, 1995, 37(1): 101- 117.

[3] Karl T R, Jones P D, Knight R W, et al. A new perspective on recent global warming: Asymmetric trends of daily maximum and minimum temperature. Bulletin of the American Meteorological Society, 1993, 74(6): 1007-1023.

[4] Cooter E J, LeDuk S K. Recent frost data trends in the northern United States. International Journal of Climatology, 1993, 15(1): 65-75.

[5] Gruaz G, Rankova E, Razuvaev V. Indictors of climatechange for the Russian federation. Climatic Change, 1999, 42(2): 219-242.

[6] Frich P, Alexander L V, Della-Marta P, et al. Observed coherent changes in climate extremes during the second half of the 20th century. Climate Research, 2002, 19(1): 193 -212.

[7] 任福民,翟盘茂. 1951-1990 年中国极端温度变化分析. 大气科学, 1998, 22(2): 217-227.

[8] Zhai P M, Sum A J, Ren Fumin, et al. Changes of climate extremes in China. Climatic Change, 1999, 42: 203-218.

[9] 马柱国, 符宗斌, 任小波, 等. 中国北方年极端温度的变化趋势与区域增暖的联系. 地理学报, 2003, 58(S1): 11-20.

[10] 翟盘茂, 潘晓华. 中国北方近50 年温度和降水极端事件变化. 地理学报, 2003 , 58(S1): 1- 10.

[11] 龚道溢, 韩晖. 华北农牧交错带夏季极端气候的趋势分析. 地理学报, 2004, 59(2): 230-238.

[12] 苗爱梅, 武捷, 贾利冬. 1958-2008 年山西气温变化的特征及趋势研究. 地球科学进展, 2010, 25(3): 264-272.

[13] 王海军, 张勃, 赵传燕, 等.中国北方近57 年气温时空变化特征. 地理科学进展, 2009, 28(4): 643-650

[14] 王学锋, 周德丽, 杨鹏武. 近48 年来城市化对昆明地区气温的影响. 地理科学进展, 2010, 29(2): 145-150

[15] 李克让, 林贤超, 王维强. 近四十年来我国气温的长期变化趋势. 地理研究, 1990, 9(4): 26-37.

[16] 宋连春. 近40 年我国气温时空变化特征.应用气象学报. 1994, 5(1): 119-124.

[17] 翟盘茂, 任福民.中国近四十年最高最低温度变化. 气象学报, 1997, 55(4): 418-429.

[18] 陈隆勋, 朱文琴. 中国近45年来气候变化的研究. 气象学报, 1998, 56(3): 257-271.

[19] 屠其璞, 邓自旺, 周晓兰. 中国气温异常的区域特征研究. 气象学报, 2000, 58(3): 288-296.

[20] 沙万英, 邵雪梅, 黄玫. 20 世纪80 年代以来中国的气候变暖及其对自然区域界线的影响. 中国科学: D 辑, 2002, 32(4): 317-326.

[21] 任国玉, 徐铭志, 初子莹, 等.近54 年中国地面气温变化. 气候与环境研究, 2005, 10(4): 717-727.

[22] 唐国利, 任国玉. 近百年中国地表气温变化趋势的再分析. 气候与环境研究, 2005, 10(4): 791-797.

[23] 钱维宏, 符娇兰, 张玮玮, 等.近40 年中国平均气候与极值气候变化的概述. 地球科学进展, 2007, 23(7): 674-683.

[24] 王鹏祥, 杨金虎, 张强, 等. 近半个世纪来中国西北地面气候变化基本特征. 地球科学进展, 2007, 23(6): 650-655.

[25] 周天军, 赵宗慈. 20 世纪中国气候变暖的归因分析. 气候变化研究进展, 2006, 2(1): 28-32.

[26] 邓振镛, 张强, 徐金芳, 等. 高温热浪与干热风的危害特征比较研究. 地球科学进展, 2009, 24(8): 865-873.

[27] 朱乾根, 林锦瑞, 寿绍文, 等. 天气学原理和方法. 北京: 气象出版社, 1993: 40.
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