中国农业气象 ›› 2026, Vol. 47 ›› Issue (6): 813-826.doi: 10.3969/j.issn.1000-6362.2026.06.001

• 农业气候资源与气候变化栏目 •    下一篇

甘肃省气象干旱时空变化对气候因素变化的响应

马亚丽,牛最荣,张彦洪   

  1. 甘肃农业大学水利水电工程学院,兰州730070
  • 收稿日期:2025-05-21 出版日期:2026-06-20 发布日期:2026-06-18
  • 基金资助:
    甘肃省引大入秦水资源利用中心项目(GSAU−JSFW−2026−04);国家自然科学基金项目(42261003);甘肃省水利厅项目(GSAU−JSFW−2024−74);甘肃省水利科学试验研究及技术推广项目(25GSLK077)

Response of Spatiotemporal Variations of Meteorological Drought to Changes in Climatic Factors in Gansu Province

MA Ya-li, NIU Zui-rong, ZHANG Yan-hong   

  1. College of Water Conservancy and Hydropower Engineering, Gansu Agricultural University, Lanzhou 730070, China
  • Received:2025-05-21 Online:2026-06-20 Published:2026-06-18
  • About author:马亚丽,讲师,主要从事水文与水资源研究,E-mail:gsaumayl@163.com

摘要:

基于甘肃省地面监测气象站实测资料,采用标准化降水蒸发指数(SPEI探讨19842019年甘肃省气象干旱年、季尺度时空演变特征,利用散点图及相关系数揭示干旱变化与气候要素的相关关系,选取Gumbelcopula函数构建甘肃省年尺度SPEI和降水量的联合分布模型,探讨并识别干旱时空演变特点及驱动气候要素,明确降水事件对该地区干湿变化的影响。结果表明:(119842019年甘肃省降水量(P)增加变化不显著,平均气温(T)呈显著上升趋势,潜在蒸散发(ET0)呈显著增加变化。(2)甘肃省年尺度干旱指数呈不显著下降趋势,多年呈趋干变化,总体干旱趋势趋于平稳。河西地区多年出现干旱的程度较甘肃其他地区严重,张掖一带多年干旱程度最严重。3)四季干旱程度排序为春季>夏季>秋季>冬季。河西地区夏季、秋季干旱程度比春季、冬季严重,陇东地区、陇南地区表现为春季、冬季干旱程度较严重。(4)研究期内全省降水量增加,发生较轻干旱的可能性增大,年尺度SPEI与降水量同时出现最大值的可能性为91.60%,具有高度相关关系,且发生轻旱、中旱、重旱和特旱最大值的可能性分别为80.38%61.15%38.62%18.81%

关键词: 甘肃省, 气象干旱, 时空变化, 气候要素, 响应特征

Abstract:

Based on the measured data from ground monitoring meteorological stations in Gansu province, this paper used the standardized precipitation evaporation index (SPEI) to explore the temporal and spatial evolution characteristics of meteorological drought at the annual and seasonal scales in Gansu. Scatter plots and correlation coefficients were used to reveal the correlation between drought changes and climatic factors. The Gumbel−copula function was selected to construct a joint distribution model of SPEI and precipitation at the annual scale in Gansu province, to explore and identify the spatio−temporal evolution characteristics of drought and the driving climatic factors, and to clarify the possibility of precipitation influencing dry and wet changes. The results showed that: (1) from 1984 to 2019, the change in precipitation (P) was not significant, while the average temperature (T) showed a significant upward trend, and potential evapotranspiration (ET0) showed a significant increase in Gansu province. (2) The annual−scale drought index in Gansu showed a non−significant downward trend, and it tended to become drier over the years. The overall drought trend tended to be stable. The severity of drought in the Hexi region was more severe than in other areas of Gansu province, and the area around Zhangye had suffered the most severe droughts for many years. (3) The order of drought severity in the four seasons was spring, summer, autumn and winter. The drought in spring was the most severe. The drought severity in the Hexi region was more severe in summer and autumn than in spring and winter, while the Longdong region and Longnan region showed more severe drought in spring and winter. (4) During the research period, the increase in precipitation across the province had raised the possibility of less severe droughts. The possibility of the maximum values of annualscale SPEI and precipitation occurring simultaneously was 91.60%, showing a high degree of correlation. The maximum possibilities of light drought, moderate drought, severe drought and extreme drought were 80.38%, 61.15%, 38.62% and 18.81%, respectively. 

Key words: Gansu province, Meteorological drought, Spatiotemporal variation, Climatic factor, Response characteristics