干旱区研究 ›› 2018, Vol. 35 ›› Issue (1): 68-76.doi: 10.13866/j.azr.2018.01.09 cstr: 32277.14.AZR.20180109

• 天气与气候 • 上一篇    下一篇

近54 a中国西北地区气温和降水的时空变化特征

商沙沙1, 廉丽姝2, 马婷1, 张琨1, 韩拓1   

  1. 1.兰州大学资源环境学院西部环境教育部重点实验室, 甘肃 兰州 730000;
    2.曲阜师范大学地理与旅游学院, 山东 曲阜 276826
  • 收稿日期:2017-02-27 修回日期:2017-06-06 出版日期:2018-01-15 发布日期:2018-02-06
  • 通讯作者: 廉丽姝.E-mail:llsh8210@163.com
  • 作者简介:商沙沙(1994-),女,在读硕士研究生,主要从事干旱区水文过程研究.E-mail:shangshsh16@lzu.edu.cn
  • 基金资助:
    国家重点研发计划资助(2016YFC0500203);国家自然基金项目(31370467 and 41571016);中央高校基本科研业务费专项资金(lzujbky-2015-862151)资助

Spatiotemporal Variation of Temperature and Precipitation in Northwest China in Recent 54 Years

SHANG Sha-sha1, LIAN Li-shu2, MA Ting1, ZHANG Kun1, HAN Tuo1   

  1. 1. Key Laboratory of Environmental Education in West China of the Ministry of Education,Lanzhou University,Lanzhou 730000,Gansu,China;
    2. College of Geography and Tourism,Qufu Normal University,Qufu 276826,Shandong,China
  • Received:2017-02-27 Revised:2017-06-06 Published:2018-01-15 Online:2018-02-06

摘要: 利用中国西北地区1961—2014年191个台站的逐月气温和降水资料,通过线性倾向估计、滑动平均、累积距平、IDW(反距离空间插值)等方法,研究了西北地区气温和降水的时空变化特征。结果表明:近54 a西北地区平均气温呈波动上升趋势,其中冬季的增温速率最大,极端最高、最低气温均呈上升趋势。降水量也呈上升趋势,尤其是近几年上升速度较快。降水主要集中在夏季,进入21世纪后冬季降水增加。多年平均气温较高区域集中在南疆地区、祁连山东南部,其中升温较明显区域集中在准噶尔盆地和天山地区西南部分地区。降水量表现出东多西少的特征,降水量较多区域集中在祁连山东南部,降水量较少区域集中在南疆地区,其中降水增加较明显区域集中在北疆地区、塔里木盆地的西部地区。从西北地区近54 a气温和降水的时空变化可以看出,西北地区有向暖湿转变的趋势。

关键词: 气温, 降水量, 气候变化, 时空特征, 西北地区

Abstract: Based on the temperature and precipitation data from 191 meteorological stations in northwest China during the period from 1961 to 2014,many methods,such as the linear trend,running means,accumulative anomaly and IDW,were used to study the spatiotemporal variation of temperature and precipitation in northwest China. The results showed that the average temperature was in an increase trend,especially in winter.The trend of extreme maximum temperature and extreme minimum temperature was similar to that of average temperature.Precipitation was also in an increase trend,especially in recent years.Precipitation occurred mainly in summer,in particular,the precipitation in winter increased sharply since the 21st century.The high annual temperature occurred mainly in south Xinjiang and the southeast Qilian Mountains,especially in the Junggar Basin and the southwest Tianshan Mountains.Precipitation decreased gradually from the east to the west.More precipitation occurred in the southeast Qilian Mountains,and its low value occurred in south Xinjiang.Precipitation increase was significant in the west Tarim Basin and north Xinjiang.Viewing from the spatiotemporal variation of temperature and precipitation,there was a warming-wetting trend in northwest China.

Key words: temperature, precipitation, climate change, spatiotemporal variation, northwest China