extreme temperature,cold(warm) index,index; spatiotemporal variation,Hedong region, Gansu Province ,"/> 近30 a河东地区极端气温时空变化

干旱区研究 ›› 2019, Vol. 36 ›› Issue (6): 1466-1477.

• 应用气候 • 上一篇    下一篇

近30 a河东地区极端气温时空变化

焦文慧1,张勃1,黄涛2,马尚谦1,候启1   

  1. 1.西北师范大学地理与环境科学学院,甘肃 兰州 7300702.西北区域气候中心,甘肃 兰州 730020
  • 收稿日期:2019-01-07 修回日期:2019-03-07 出版日期:2019-11-15 发布日期:2019-11-15
  • 通讯作者: 张勃
  • 作者简介:焦文慧(1995-),女,硕士,主要从事区域环境与资源开发研究.E-mail:jiaowenhuixlt@163.com
  • 基金资助:
    国家自然科学基金项目(41561024)资助

Spatiotemporal Change of Extreme Temperature in the Hedong Region in Recent 30 Years

JIAO Wen-hui1, ZHANG Bo1, HUANG Tao2, MA Shang-qian1, HOU Qi1   

  1. 1. College of Geography and Environment Science, Northwest Normal University, Lanzhou 730070, Gansu, China;
    2. Northwest Regional Climate Center, Lanzhou 730020, Gansu, China

  • Received:2019-01-07 Revised:2019-03-07 Online:2019-11-15 Published:2019-11-15

摘要: 利用61个气象站1988—2017年逐日最高气温、最低气温和平均气温资料,采用线性倾向估计、Mann-Kendal检验、滑动t以及相关分析方法,对河东地区极端气温事件的时空变化特征进行研究,结果表明:①河东地区近30 a日最高气温的极大(小)值、日最低气温的极大(小)值、年平均最高(低)气温、夏日日数、热夜日数、暖昼(夜)日数、气温日较差、暖日持续日数、生物生长季呈现增大(加)趋势,霜冻日数、冰冻日数、冷昼(夜)日数、冷日持续日数呈现减小(少)趋势;②暖指数的变暖幅度大于冷指数,昼指数的变暖幅度大于夜指数,陇东高原地区变暖幅度最大,甘南高原地区变暖幅度最小;③多数指数的突变点在20世纪90年代中后期和21世纪初期;④多数极端气温指数与经度和海拔高度显著相关,河东地区极端气温指数的变化与区域性增暖有密切联系。

关键词: 极端气温, 冷(暖)指数, 时空变化, 河东地区, 甘肃

Abstract: The methods of linear regression, Mann-Kendal test, sliding T-test and correlation analysis were used to analyze the spatiotemporal variation of extreme temperature events in the Hedong region based on the daily temperature (maximum, minimum and average) data from 61 meteorological stations in the study area during the period of 1988-2017. The results showed that: ①In recent 30 years, the daily maximum and minimum temperature values, annual mean maximum and minimum temperature values, summer duration, tropical nights, warm days, warm nights, daily temperature range, warm-day duration and growing season were in an increase trend. Whereas the frost days, ice days, cold days, cold nights and cold-day duration were in a decrease trend; ② The change ranges of warming indices were obviously higher than those of cold ones. The warming ranges of diurnal indices were higher than those of nocturnal ones. The warming range was the highest in the Loess Plateau in east Gansu Province but the lowest in the Gannan Plateau; ③ Abrupt change of the most temperature indices occurred in the mid-1990s and early 21st century; ④ Most extreme temperature indices were closely related to the longitude and altitude. The variation of extreme temperature indices in the Hedong region was closely related to the regional warming.

Key words: extreme temperature')">

extreme temperature, cold(warm) index, index; spatiotemporal variation, Hedong region, Gansu Province