植被对土壤湿度与饱和水汽压亏缺响应的阈值量化OA
Threshold quantification of vegetation response to soil moisture and vapor pressure deficits
本文探讨了多源土壤数据下骤旱特征的空间分布,基于二维copula方法量化了骤旱背景下导致太阳诱导叶绿素荧光下降的土壤湿度和饱和水汽压亏缺阈值,并分析其在中国不同干湿区、植被类型下的空间异质性.结果表明:2001-2020年间北方地区骤旱频次为8次以下,历时在10候以上,强度多为3~4级,南方地区为8次以上,历时约6~10候,强度多为1~2级.在土壤湿度主导区内触发SIF≤SIF40%的土壤湿度阈值,湿润区、半湿润区、半干旱区、干旱区分别约为0.39 m3m-3、0.35 m3m-3、0.25 m3m-3、0.06 m3m-3,森林、农田、草地分别约为0.38 m3m-3、0.35 m3m-3、0.28 m3m-3.在饱和水汽压亏缺主导区内,其阈值在干旱区、湿润和半湿润区、半干旱区分别约为7 hPa、4 hPa和2.5 hPa,在农田、森林、草地分别约为5 hPa、4 hPa、3 hPa.
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.
孟长青;李月;王永强;王远坤;张验科
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华北电力大学 水利与水电工程学院,北京 102206长江水利委员会 长江科学院,武汉 430010华北电力大学 水利与水电工程学院,北京 102206华北电力大学 水利与水电工程学院,北京 102206
天文与地球科学
骤旱土壤湿度饱和水汽压亏缺Copula植被阈值
flash droughtsoil moisturevapor pressure deficitCopulavegetationthreshold
《水力发电学报》 2026 (3)
24-34,11
国家自然科学基金项目(525790104190102852279064)
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