中国农业气象 ›› 2026, Vol. 47 ›› Issue (10): 1704-1718.doi: 10.3969/j.issn.1000-6362.2026.10.014

• 农业气象灾害栏目 • 上一篇    下一篇

基于XGBoost算法的1912−1949年陕西气象干旱重建及时空变化特征

丁梅,吕娟,屈艳萍   

  1. 1. 中国水利水电科学研究院流域水循环与水安全全国重点实验室/水利部防洪抗旱减灾技术创新中心,北京 100038; 2. 北京市密云区应急管理局,北京 101599
  • 收稿日期:2026-05-19 出版日期:2026-10-20 发布日期:2026-10-19
  • 作者简介:丁梅,E-mail:dingmei9553@163.com
  • 基金资助:
    国家重点研发计划课题(2023YFC3006604);中国水利水电科学研究院基本科研业务费专项项目(JZ110145B0192026;JZ110145B0082026)

Reconstruction and Spatiotemporal Variation Characteristics of Meteorological Drought in Shaanxi Province from 1912 to 1949 Based on the XGBoost Algorithm

DING Mei, LV Juan, QU Yan-ping   

  1. 1.State Key Laboratory of Water Cycle and Water Security, China Institute of Water Resources and Hydropower Research/Technology Innovation Center for Flood and Drought Prevention and Disaster Reduction, China Institute of Water Resources and Hydropower Research, Beijing 100038, China; 2.Miyun District Emergency Management Bureau of Beijing Municipality, Beijing 101599
  • Received:2026-05-19 Online:2026-10-20 Published:2026-10-19

摘要:

利用1981−2019年陕西9个气象观测站数据与英国东英格利亚大学气候研究中心发布的CRU TS v4.09逐月格点气候数据集,引入XGBoost机器学习算法,以1981−2010年为训练期,2011−2019年为测试期,构建陕西水热气象数据订正模型,用于订正1912−1949年陕西CRU TS v4.09逐月格点水热气象数据,结合标准化降水蒸散指数(SPEI)重建1912−1949年陕西气象干旱指数,进而分析陕西气象干旱时空演变特征,以期为区域历史干旱重建提供参考。结果表明:(1)基于XGBoost机器学习算法构建的水热气象数据订正模型,其订正效果良好,测试期内降水量区域平均R2为0.77,RMSE为29.27mm,平均气温区域平均R2为0.92,RMSE为2.08℃;(2)基于水热气象数据订正模型,订正了1912−1949年陕西CRU TS v4.09逐月格点水热气象数据,据此1912−1949年陕西降水量呈北增南降的弱波动特征,变化趋势不显著;陕西平均气温呈显著上升趋势(P<0.05),水热要素的演变非协同变化;(3)1912−1921年陕西干旱覆盖率与干旱强度偏低,1922−1949年攀升并呈多峰振荡特征,1941年干旱覆盖率与干旱强度达到全域峰值;(4)1912−1949年陕西干旱发生频率由南向北递增,干旱强度由南向北递减,高等级干旱高频区集中于关中和陕南部分区域;(5)1912−1949年陕西干旱化整体加剧,陕南干旱化趋势具有显著性。综上,XGBoost机器学习算法可较好地支撑历史格点气象数据订正工作,可为长序列历史气象干旱重建及演变分析提供参考。

关键词: 气象数据订正, 干旱重建, SPEI指数, 时空演变

Abstract:

Based on observational data from 9 meteorological stations in Shaanxi province and the CRU TS v4.09 monthly grid climate dataset released by the Climate Research Centre of the University of East Anglia in the United Kingdom from 1981 to 2019, the XGBoost machine learning algorithm was introduced. Taking 1981−2010 as the training period and 2011−2019 as the testing period, a machine learning correction model was established. A correction was applied to the hydrothermal meteorological data from the CRU TS v4.09 monthly grid climate data set for Shaanxi province from 1912 to 1949. Combined with the Standardized precipitation evapotranspiration index (SPEI), the meteorological drought index of Shaanxi from 1912 to 1949 was reconstructed, and the spatiotemporal evolution characteristics of meteorological droughts were analyzed to provide a reference for regional historical drought reconstruction. The results showed that: (1) the hydrothermal meteorological correction model constructed by the XGBoost algorithm exhibited satisfactory simulation performance, with precipitation R2 of 0.77 and RMSE of 29.27mm, and mean temperature R2 of 0.92 and RMSE of 2.08℃ during the testing period. (2) Based on the hydrothermal meteorological correction model, the monthly grid based hydrothermal meteorological data of CRU TS v4.09 in Shaanxi province from 1912 to 1949 were corrected. From 1912 to 1949, precipitation in Shaanxi showed a slightly fluctuating pattern of increasing in the north and decreasing in the south, with a nonsignificant trend. The mean temperature exhibited an extremely significant increasing trend (P<0.05). (3) The drought coverage and intensity in Shaanxi were relatively low from 1912 to 1921, but rose from 1922 to 1949 and showed a characteristic of multi peak oscillation. In 1941, the drought coverage and intensity reached the peak of the entire region. (4) From 1912 to 1949, drought frequency increased while drought intensity decreased from south to north across the province. High-frequency areas of severe drought were mainly distributed in Guanzhong and parts of southern Shaanxi. (5) The overall drought tendency of Shaanxi intensified from 1912 to 1949, and southern Shaanxi witnessed the most significant trend. In summary, the XGBoost algorithm can effectively correct historical gridded meteorological data, providing technical support and methodological reference for the reconstruction and evolution analysis of long−term historical meteorological droughts.

Key words: Meteorological data correction, Drought reconstruction, SPEI index, Spatiotemporal evolution