气候变化研究进展 ›› 2025, Vol. 21 ›› Issue (3): 317-326.doi: 10.12006/j.issn.1673-1719.2024.276

• 气候系统变化 • 上一篇    下一篇

气候水文预估不确定性量化及约束方法研究进展

张琴1,2,3(), 张利平2(), 李意4, 刘丽娜2, 佘敦先2, 周芷菱2, 袁喆1,3   

  1. 1.长江水利委员会长江科学院,武汉 430010
    2.武汉大学水资源工程与调度全国重点实验室,武汉 430072
    3.流域水资源与生态环境科学湖北省重点实验室,武汉 430010
    4.中国电建集团贵阳勘测设计研究院有限公司,贵阳 550081
  • 收稿日期:2024-10-25 修回日期:2024-12-19 出版日期:2025-05-30 发布日期:2025-04-18
  • 通讯作者: 张利平,男,教授,zhanglp@whu.edu.cn
  • 作者简介:张琴,男,工程师,zhangqinwhu@whu.edu.cn
  • 基金资助:
    中央级公益性科研院所基本科研业务费项目(CKSF2024989/SZ);国家自然科学基金项目(52279023);武汉市自然科学基金特区计划项目(2024040701010035);工程二三维GIS勘测设计系统关键技术研究(KY94200004)

Research progress on uncertainty quantification and constraint methods for climate and hydrological projections

ZHANG Qin1,2,3(), ZHANG Li-Ping2(), LI Yi4, LIU Li-Na2, SHE Dun-Xian2, ZHOU Zhi-Ling2, YUAN Zhe1,3   

  1. 1. Changjiang River Scientific Research Institute, Changjiang Water Resources Commission, Wuhan 430010, China
    2. State Key Laboratory of Water Resources Engineering and Management, Wuhan University, Wuhan 430072, China
    3. Hubei Key Laboratory of Water Resources & Eco-Environment Science, Wuhan 430010, China
    4. Guiyang Engineering Co., Ltd., China Electric Power Construction Group, Guiyang 550081, China
  • Received:2024-10-25 Revised:2024-12-19 Online:2025-05-30 Published:2025-04-18

摘要:

准确量化并减小气候水文预估的不确定性是后续气候变化影响评估和适应性策略制定的前提。针对预估不确定性的分离量化,系统回顾了不同方法的发展历程,陈述了方法的实现过程和适用情况,包括HS09法、L20法和方差分析法。进一步阐明了减小模式不确定性的必要性和思路,将约束预估方法分为4类:检测归因约束、加权约束、涌现约束和校正约束,全面介绍了各个方法的原理,从关系的建立、适用尺度、应用变量等多方面分析了约束方法的特性和优缺点,随后总结了不同约束方法的检验及结果评估的实现流程。最后展望了该领域亟需关注的重点内容和未来可能的发展趋势,以期为提高气候水文变量或极端事件预估的准确性和可靠性提供参考。

关键词: 气候变化, 气候模式, 预估不确定性, 约束预估, 涌现约束, 完美模型检验

Abstract:

Accurately quantifying and reducing the uncertainty of climate and hydrological projections is a prerequisite for subsequent climate change impact assessment and adaptation strategy development. For the quantification of projection uncertainty, the development history of different methods is systematically reviewed, and the realization process and applicability of methods, including the HS09, the L20, and the analysis of variance are stated. Further the necessity and ideas to reduce the model uncertainty are elucidated, and the constraint projection methods are classified into four categories: detecting attribution constraints, weighting constraints, emergent constraints, and correction constraints. The principle of each method are comprehensively introduced, and the characteristics of the constraint methods in terms of the establishment of the relationship, the applicability of the scales and variables, are analyzed. Then the implementation process of testing different constraint methods and evaluating the results are summarized. Finally, the key points that need urgent attention in this field are discussed, and the possible future trends are prospected, with a view to providing reference for improving the accuracy and reliability of climate and hydrological variables projections.

Key words: Climate change, Climate model, Uncertainty of projection, Constraint projection, Emergent constraint, Perfect Model Test

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