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植被对土壤湿度与饱和水汽压亏缺响应的阈值量化

孟长青 李月 王永强 王远坤 张验科

水力发电学报2026,Vol.45Issue(3):24-34,11.
水力发电学报2026,Vol.45Issue(3):24-34,11.DOI:10.11660/slfdxb.20260303

植被对土壤湿度与饱和水汽压亏缺响应的阈值量化

Threshold quantification of vegetation response to soil moisture and vapor pressure deficits

孟长青 1李月 2王永强 3王远坤 2张验科2

作者信息

  • 1. 华北电力大学 水利与水电工程学院,北京 102206||北京怀柔实验室,北京 101499
  • 2. 华北电力大学 水利与水电工程学院,北京 102206
  • 3. 长江水利委员会 长江科学院,武汉 430010
  • 折叠

摘要

Abstract

This study explores the spatial distribution of flash drought characteristics from multi-source soil data,and quantifies the thresholds of soil moisture and vapor pressure deficit that lead to a decrease in solar-induced chlorophyll fluorescence under flash drought conditions,using a two-dimensional copula method.We also examines the thresholds'spatial heterogeneity in different aridity zones and different vegetation types across China.The results show that in the period of 2001-2020,the northern region experienced flash droughts less than 8 times,lasting over 10 pentads,with intensities mostly at Levels 3-4.In contrast,the southern region experienced more than 8 times,lasting about 6-10 pentads,with intensities mostly at Levels 1-2.For soil moisture-dominated region,the soil moisture thresholds for SIF≤SIF40%are roughly 0.39 m3m-3,0.35 m3m-3,0.25 m3m-3,and 0.06 in the humid,sub-humid,semi-arid,and arid zones,respectively,and 0.38 m3m-3,0.35 m3m-3,and 0.28 m3m-3 for forests,croplands,and grasslands,respectively.In vapor pressure deficit-dominated regions,the thresholds are around 7 hPa,4 hPa,and 2.5 hPa in arid,humid and sub-humid,and semi-arid zones,respectively,and 5 hPa,4 hPa,and 3 hPa for croplands,forests,and grasslands,respectively.

关键词

骤旱/土壤湿度/饱和水汽压亏缺/Copula/植被/阈值

Key words

flash drought/soil moisture/vapor pressure deficit/Copula/vegetation/threshold

分类

天文与地球科学

引用本文复制引用

孟长青,李月,王永强,王远坤,张验科..植被对土壤湿度与饱和水汽压亏缺响应的阈值量化[J].水力发电学报,2026,45(3):24-34,11.

基金项目

国家自然科学基金项目(52579010 ()

41901028 ()

52279064) ()

水力发电学报

1003-1243

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