湖北农业科学 ›› 2022, Vol. 61 ›› Issue (15): 25-33.doi: 10.14088/j.cnki.issn0439-8114.2022.15.005

• 资源·环境 • 上一篇    下一篇

新疆气温季节变化时空分布特征研究

叶尔克江·霍依哈孜1, 阿吉古丽·沙依提2, 买买提艾力·买买提依明3, 阿帕尔·肉孜1   

  1. 1.昌吉回族自治州气象局,新疆 昌吉 831100;
    2.新疆气象学会,乌鲁木齐 830002;
    3.中国气象局乌鲁木齐沙漠气象研究所,乌鲁木齐 830002
  • 收稿日期:2021-07-31 出版日期:2022-08-10 发布日期:2022-08-25
  • 通讯作者: 阿帕尔·肉孜(1978-),男,高级工程师,主要从事气候变化研究,(电话)0994-8165713(电子信箱)apar-ek@sohu.com。
  • 作者简介:叶尔克江·霍依哈孜(1979-),女,工程师,主要从事应用气象研究工作,(电话)0994-8166186(电子信箱)erke-ap@sohu.com
  • 基金资助:
    中央级公益性科研院所基本科研业务费专项(IDM2021005,IDM2021001); 中国气象局创新发展专项(CXFZ2021J044-03); 国家自然科学基金面上项目(41875023); 昌吉回族自治州庭州青年计划项目(2021QN28)

Study on temporal and spatial distribution characteristics of seasonal variation of air temperature in Xinjiang

ERKEJAN Hoyhazi1, AJIGUL Sayit2, MAMTIALI Mamtiyimin3, APAR Ruzi1   

  1. 1. Changji Hui Autonomous Prefecture Meteorological Burea,Changji 831100,Xinjiang,China;
    2. Xinjiang Meteorological Society, Urumqi 830002, China;
    3. Urumqi Institute of Desert Meteorology, China Meteorological Administration, Urumqi 830002,China
  • Received:2021-07-31 Online:2022-08-10 Published:2022-08-25

摘要: 基于1961—2018年新疆105个气象站点的气温资料,运用气候倾向率、Mann-Kendall检验以及ArcGIS 10.7环境下的反距离加权(IDW)插值技术,探究新疆各季度平均气温的变化趋势、突变特征以及精细化时空分布规律。结果表明,新疆各季度多年平均气温空间分布总体表现为南疆高、北疆低,平原和盆(谷)地高、山区低的格局。新疆各季度近58 a平均气温均呈逐年上升趋势,其中春季气温在2011年突变性地增温,夏季气温在2003年突变,秋季气温在1994年突变,冬季气温在1985—1986年突变;各季度均呈先下降后持续上升的趋势,但不同季节、不同地区升温幅度不同,春季、秋季和冬季北疆气温增温速率最快,夏季天山山区增温速率最快,春季、夏季和秋季南疆气温增温速率最慢,冬季天山山区气温增温速率最慢,都通过显著性检验。新疆地区各季度平均气温增温速率由北向南递减,北部增温速率大于东北部,东北部大于中部,中部大于南部,南部大于东部,这表明寒冷地区增温快于温暖地区。

关键词: 季节变化, 气候倾向率, 突变, 反距离权重插值, 时空分布

Abstract: Based on the temperature data of 105 meteorological stations in Xinjiang from 1961 to 2018, this paper used climate tendency rate, Mann Kendall test and inverse distance weighted (IDW) interpolation technology under ArcGIS10.7 environment to explore the change trend, mutation characteristics and refined spatial-temporal distribution of quarterly average temperature in Xinjiang. The results showed the overall spatial distribution of each quarter was high in South Xinjiang, low in North Xinjiang, high in the plain and basin (valley), and low in the mountain area. The average temperature of Xinjiang region in recent 58 years showed an upward trend year by year, the spring temperature increased abruptly in 2011, the summer temperature changed abruptly in 2003, the autumn temperature changed abruptly in 1994, and the winter temperature changed abruptly in 1985—1986. The temperature in each quarter showed a downward trend and then continued to rise, but the warming range was different in different seasons and regions. The warming rate was the fastest in Northern Xinjiang in spring, autumn and winter, the fastest in Tianshan Mountain area in summer, the slowest in Southern Xinjiang in spring, summer and autumn, and the slowest in Tianshan Mountain area in winter, which passed the significance test. The average temperature increasing rate of each season in Xinjiang decreased from north to south. The temperature increasing rate in the north was greater than that in the northeast, the northeast was greater than that in the middle, the middle was greater than that in the south, and the south was greater than that in the east. This showed that the temperature increasing rate in cold regions was faster than that in warm regions.

Key words: seasonal variation, climate tendency rate, mutation, inverse distance weighted, spatiotemporal distribution

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