中国农业气象 ›› 2025, Vol. 46 ›› Issue (7): 1026-1038.doi: 10.3969/j.issn.1000-6362.2025.07.011

• 农业气象灾害栏目 • 上一篇    下一篇

基于像元化SPEI的新疆气象干旱时空变化特征

易科帆,吝海霞,秦国鹏,姚宁,高雪慧,鲁伟娟,卢宇航,刘健   

  1. 1.石河子大学水利建筑工程学院/现代节水灌溉兵团重点实验室/兵团农业水肥高效关键装备技术创新中心,石河子 832000;2.西北农林科技大学水利与建筑工程学院,杨凌 712100
  • 收稿日期:2024-08-19 出版日期:2025-07-20 发布日期:2025-07-20
  • 作者简介:易科帆,E-mail:13199820855@163.com
  • 基金资助:
    第三次新疆综合科学考察项目(2022xjkk0500);伊犁哈萨克自治州科技计划项目(YZ2023A17);石河子大学高层次人才科研启动项目(2022ZK010)

Spatiotemporal Variation Characteristics of Meteorological Drought in Xinjiang Based on Pixel−scale SPEI

YI Ke-fan, LIN Hai-xia, QIN Guo-peng, YAO Ning, GAO Xue-hui, LU Wei-juan, LU Yu-hang, LIU Jian   

  1. 1. College of Water Conservancy & Architectural Engineering, Shihezi University/Key Laboratory of Modern Water-Saving Irrigation of Xinjiang Production & Construction Group/Technology Innovation Center for Agricultural Water and Fertilizer Efficiency Equipment of Xinjiang Production & Construction Corps, Shihezi 832000, China; 2. College of Water Resources and Architectural Engineering, Northwest Agriculture and Forestry University, Yangling 712100
  • Received:2024-08-19 Online:2025-07-20 Published:2025-07-20

摘要:

基于1981−2018年中国区域地面气象要素驱动数据集,计算新疆不同时间尺度的标准化降水蒸散发指数(SPEI),采用Mann−KendallMK)检验、Sen's slope方法分析新疆地区气象干旱的变化趋势、发生频率和持续时间等时空变化特征,以期为新疆地区干旱防范提供依据。结果表明:119812018新疆呈非显著干旱化趋势,受旱面积比例以0.845个百分点·10a–1速率呈非显著减少趋势。新疆春、夏季非显著干旱化趋势2005秋季干旱显著加剧,1997年后冬季趋向湿润化。(2新疆SPEI3季节性干旱的空间分布区域性明显春、夏和秋季有显著的干旱化区域,旱情加剧区域主要分布在塔里木盆地和少数地区冬季57.82%的地区呈非显著湿润化趋势,29.23%的地区呈显著湿润化,仅0.03%的地区呈显著干旱趋势,其余地区干旱趋势并不显著;(3)新疆月、季、年尺度干旱发生频率空间分布特征较一致,东部地区为干旱发生高值区年尺度干旱平均发生频率为36.05%,其中吐鲁番地区干旱频率为44.97%。新疆不同年代际干旱历时差异较小,20002009平均干旱历时最长,为3.6个月。总之,38a新疆南部和东部地区干旱化趋势严重,且干旱发生频率高,亟需加强应对措施以减轻干旱带来的不利影响。

关键词: 气象干旱, SPEI, 多时间尺度, 时空变化特征, 新疆

Abstract:

Based on the 19812018 China meteorological forcing dataset, the standardized precipitation evapotranspiration index (SPEI) was calculated for different time scales. The Mann−kendall (MK) test and Sen's slope method were used to analyze the spatial and temporal characteristics of meteorological drought in Xinjiang, including trends of change, frequency of occurrence and duration. This study endeavored to provide a scientific basis for the formulation of strategies for drought prevention and mitigation in Xinjiang. Results showed that: (1) from 1981 to 2018, the climate of Xinjiang exhibited a nonsignificant trend of aridification, with the proportion of droughtaffected area decreasing at a rate of 0.845 percentage points per decade in a non−significant manner. Both spring and summer climates showed a nonsignificant trend of aridification, while autumn meteorological droughts significantly intensified after 2005 and winter had tended to become wetter after 1997. (2) The spatial distribution of seasonal drought based on the SPEI3 in Xinjiang was regionally distinct. Significant droughtaffected areas were observed in spring, summer and autumn, with the intensified drought concentrated in the Tarim basin and a few eastern regions. During the winter, 57.82% of the area in Xinjiang exhibited a nonsignificant trend of wetting, 29.23% showed a significant trend of wetting, and only 0.03% showed a significant drought trend. The remaining areas showed a nonsignificant drought trend. (3) The spatial distribution of drought frequency at monthly, seasonal, and annual scales was relatively consistent, with the eastern region being a highfrequency drought zone. The average annual frequency of drought was 36.05%, with Turpan reaching 44.97%. Interdecadal differences in drought duration across Xinjiang were minimal, with the longest average drought duration observed in 20002009, which lasted 3.6 months. Generally, trends of aridification have intensified in the southern and eastern regions of Xinjiang over the past 38 years, with a high frequency of droughts, there is an urgent need for measures to mitigate the adverse impacts of drought.

Key words:

 Meteorological drought, SPEI, Multiple time scales; Spatial?temporal characteristics, Xinjiang