中国农业气象 ›› 2026, Vol. 47 ›› Issue (10): 1589-1602.doi: 10.3969/j.issn.1000-6362.2026.10.005

• 农业生物气象栏目 • 上一篇    下一篇

基于深度学习降尺度方法对长江上游流域CMIP6模式平均气温和降水量的预估

李夢雨,周李磊,易红伶,谭水仙,官冬杰   

  1. 重庆交通大学智慧城市学院,重庆 400074
  • 收稿日期:2025-06-27 出版日期:2026-10-20 发布日期:2026-10-19
  • 作者简介:李夢雨,E-mail:622230100008@mails.cqjtu.edu.cn
  • 基金资助:
    国家自然科学基金青年基金项目(42201333);国家自然科学基金联合基金项目(U24A20580);国家自然科学基金面上项目(42171298);重庆市研究生科研创新项目(CYS25587)

Projections of Future Mean Temperature and Precipitation in the Upper Yangtze River Basin Based on Deep Learning Downscaling of CMIP6 Models

LI Meng-yu, ZHOU Li-lei, YI Hong-ling, TAN Shui-xian, GUAN Dong-jie   

  1. School of Smart City, Chongqing Jiaotong University, Chongqing 400074, China
  • Received:2025-06-27 Online:2026-10-20 Published:2026-10-19

摘要:

第六次国际耦合模式比较计划(CMIP6)为全球气候研究提供了系统的数据支撑,降尺度技术可解决其空间分辨率无法满足复杂地形区域的气候预估问题。本研究以长江上游流域为研究区域,基于泰勒图系统评估CMIP6下8种气候模式对基准期(2015−2020年)长江上游降水量和平均气温的模拟能力,利用深度神经网络(DNN)构建多特征融合的降尺度模型对优选的气候模式进行空间降尺度,分析未来期(2050年)SSP1−2.6、SSP2−4.5、SSP3−7.0和SSP5−8.5四种情景下长江上游降水量与平均气温的变化特征。结果表明:Ec−Earth3−Veg气候模式对2015−2020年长江上游降水量模拟能力最佳,ACCESS−ESM1−5 气候模式对2015−2020年长江上游平均气温模拟能力最佳。基于DNN构建的多特征融合空间降尺度模型,可将2015−2020年及2050年长江上游降水量水平分辨率从0.7031°×0.7018°升至0.008°×0.008°,平均气温水平分辨率从1.875°×1.250°升至0.018°×0.018°。降水量和平均气温降尺度结果与实测数据的相关系数均值分别为0.47和0.88。SSP1−2.6和SSP5−8.5排放情景2050年降水量与基准期相比显著增加,SSP2−4.5和SSP3−7.0情景下显著减少,SSP3−7.0情景减少幅度最大,为15.51%。平均气温在所有情景下均较基准期呈升高趋势,高排放情景增幅更剧烈。本研究可为长江上游流域水资源科学调配、农业生产精准管理提供数据支撑,并为区域极端气候灾害风险评估与应对策略制定提供科学参考。

关键词: 长江上游流域, CMIP6气候模式, 深度神经网络, 降尺度

Abstract:

The Coupled Model Intercomparison Project Phase 6 (CMIP6) provides systematic data support for global climate research, and downscaling techniques can address the limitation of its spatial resolution, which is insufficient for climate projections in regions with complex terrain. This study focused on the upper Yangtze River basin, systematically evaluated the simulation capabilities of eight CMIP6 climate models for precipitation and mean temperature during the baseline period (2015−2020) using Taylor diagrams, and constructed a multi−feature fusion downscaling model based on Deep Neural Networks (DNN) to downscale the optimized climate models spatially, and analyzed the variation characteristics of precipitation and mean temperature in the basin under four future scenarios (SSP1−2.6, SSP2−4.5, SSP3−7.0 and SSP5−8.5) in 2050. The results showed that the Ec−Earth3−Veg climate model performed best at simulating precipitation in the upper Yangtze River basin from 2015 to 2020, while the ACCESS−ESM1−5 model performed best at simulating mean temperature over the same period. The multi−feature fusion spatial downscaling model, based on a DNN, increased the horizontal resolution of precipitation in the region from 0.7031°×0.7018° to 0.008°×0.008° for both the 2015−2020 and 2050 periods, and the horizontal resolution of mean temperature from 1.875°×1.250° to 0.018°×0.018°. The average correlation coefficient between the downscaled precipitation and mean temperature results and the observed data was 0.47 and 0.88, respectively. Compared with the baseline period, precipitation in 2050 was projected to increase significantly under the SSP1−2.6 and SSP5−8.5 scenarios, while it was expected to decrease significantly under the SSP2−4.5 and SSP3−7.0 scenarios, with the largest decrease of 15.51% under SSP3−7.0. The mean temperature was projected to rise relative to the baseline period in all scenarios, with greater warming in the higher-emission scenarios. This study provides data to support the scientific allocation of water resources and the precise management of agricultural production in the upper Yangtze River basin. It serves as a scientific reference for risk assessment and response strategies to extreme regional climate events.

Key words: Upper Yangtze River basin, CMIP6 climate model, Deep neural network, Downscaling