水分再循环计算模型的研究进展及其展望

李修仓; 姜彤; 吴萍

doi:10.11867/j.issn.1001-8166.2020.085

地球科学进展 >

2020 , Vol. 35 >Issue 10: 1029 - 1040

DOI: https://doi.org/10.11867/j.issn.1001-8166.2020.085

综述与评述

水分再循环计算模型的研究进展及其展望

李修仓 ,
姜彤 ,
吴萍

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^1.中国气象局国家气候中心/气候研究开放实验室，北京 100081
^2.南京信息工程大学气象灾害预报预警与评估协同创新中心/灾害风险管理学院/地理科学学院，江苏南京 210044

李修仓（1982-），男，山东郓城人，高级工程师，主要从事气候变化与水循环研究. E-mail:lixiucang@cma.gov.cn

收稿日期: 2020-07-30

修回日期: 2020-09-22

网络出版日期: 2020-11-30

基金资助

国家重点研发计划项目“全球气候系统能量与水循环时空演变及其成因辨识”(2017YFA0603701);第二次青藏高原综合科学考察研究专题“亚洲水塔变化及其广域效应”(2019QZKK0208)

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Progress and Prospect of the Moisture Recycling Models

Xiucang Li ,
Tong Jiang ,
Ping Wu

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^1.National Climate Center/Laboratory for Climate Studies，China Meteorological Administration，Beijing 100081，China
^2.Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters/Institute for Disaster Risk Management/School of Geographical Sciences，Nanjing University of Information Science & Technology，Nanjing 210044，China

Li Xiucang (1982-), male, Yuncheng County, Shandong Province, Senior Engineer. Research areas include climate change and water cycle. E-mail:lixiucang@cma.gov.cn

Received date: 2020-07-30

Revised date: 2020-09-22

Online published: 2020-11-30

Supported by

the National Key Research and Development Program of China “Spatiotemporal evolution of energy and water cycle in global climate system”(2017YFA0603701);The Second Tibetan Plateau Scientific Expedition and Research Program “The change of Asian water tower and its wide effect”(2019QZKK0208)

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摘要

水分再循环是蒸发的水汽以降水的形式再次返回本地的过程，是水文大循环的重要组成部分。回顾了水分再循环基础理论的发展过程，系统地梳理了国内外3类水分再循环研究方法，分析了不同箱式分析模型边界条件和假设条件的异同，对比了水汽追踪和物理示踪等方法的优点及局限性。当前国内外水分再循环的研究存在尺度依赖性高、全球尺度研究较少等突出问题，箱式分析再循环模型有待深入比较或优化改进，应发展相对共识的等尺度计算方案；此外，水分再循环的研究应与全球水文大循环的研究相结合，包括计算或补全全球水量平衡分量，同时还应考虑水循环的动态变化问题。

关键词： 水分再循环; 蒸散发; 降水; 水汽输送; 水循环

本文引用格式

李修仓 , 姜彤 , 吴萍 . 水分再循环计算模型的研究进展及其展望[J]. 地球科学进展, 2020 , 35(10) : 1029 -1040 . DOI: 10.11867/j.issn.1001-8166.2020.085

Abstract

As an important part of the hydrological cycle， moisture recycling is a process in which evaporated water vapor returns to the local area again in the form of precipitation. In this paper， the development process of the basic theory of moisture recycling was reviewed. Three types of moisture recycling research methods from the domestic and foreign research were investigated systematically. The similarities and differences of the boundary conditions and assumptions of different box analysis models were analyzed. The advantages and limitations of water vapor tracer method and isotopic tracer method were compared. In the current domestic and international moisture recycling research， scale-dependence of the results and fewer studies on global scale are still outstanding problems. The box analysis recycling model needs to be optimized and improved. Relatively consensus equal-scale calculation schemes should be developed. In addition， moisture recycling studies should be combined with the studies of the global water cycle， in order to supplement relevant components of global water balance. Dynamic changes of the water cycle should also be considered the changes of moisture recycling.

Key words： Moisture recycling; Evapotranspiration; Precipitation; Water vapor transport; Water cycle

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