Spatiotemporal Variations of Reference Evapotranspiration and Its Determining Climatic Factors in the Taihang Mountains, China

Reference evapotranspiration (ETo) is an effective measure of atmospheric water demand of the land surface. In-depth investigations of the relationship between ETo and primary climatic factors can facilitate the adaptable agriculture and optimize water management, especially in the ecologically frag...

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Autores principales: Tingting Kang, Zeng Li, Yanchun Gao
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Lenguaje:EN
Publicado: MDPI AG 2021
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Acceso en línea:https://doaj.org/article/0b46699a01894a51a3104a25ff6243a1
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spelling oai:doaj.org-article:0b46699a01894a51a3104a25ff6243a12021-11-11T19:58:31ZSpatiotemporal Variations of Reference Evapotranspiration and Its Determining Climatic Factors in the Taihang Mountains, China10.3390/w132131452073-4441https://doaj.org/article/0b46699a01894a51a3104a25ff6243a12021-11-01T00:00:00Zhttps://www.mdpi.com/2073-4441/13/21/3145https://doaj.org/toc/2073-4441Reference evapotranspiration (ETo) is an effective measure of atmospheric water demand of the land surface. In-depth investigations of the relationship between ETo and primary climatic factors can facilitate the adaptable agriculture and optimize water management, especially in the ecologically fragile Taihang Mountains (THM). This work assessed the spatiotemporal dynamics of ETo and its driving climatic factors from 1973 to 2016 in THM. Results showed: (1) Annual ETo slightly increased during 1973–2016; relative humidity (RH) decreased more slowly, the temperature increased more rapidly, and wind speed (WS) decreased more rapidly at higher elevation than those at lower elevations; (2) two breakpoints occurred in ETo series at 1990 and 1997, and an “evaporation paradox” existed in 1973–1990; (3) ETo at higher elevations had greater sensitivity to changes in RH and lower sensitivity to changes in Tmax and WS. Sensitivity of ETo to minimum air temperature (Tmin) at middle elevations was lowest among three elevation bands; (4) RH and sunshine duration (SD) were the dominant climatic factors of ETo for most periods and stations. This study helps us understand the impact of climate change on ETo in mountainous areas and confirms reference evapotranspiration in high-elevation areas is particularly sensitive to climate change.Tingting KangZeng LiYanchun GaoMDPI AGarticlereference evapotranspirationmultiple breakpointssensitivity analysisvertical gradientsdominant climatic factormountainous areaHydraulic engineeringTC1-978Water supply for domestic and industrial purposesTD201-500ENWater, Vol 13, Iss 3145, p 3145 (2021)
institution DOAJ
collection DOAJ
language EN
topic reference evapotranspiration
multiple breakpoints
sensitivity analysis
vertical gradients
dominant climatic factor
mountainous area
Hydraulic engineering
TC1-978
Water supply for domestic and industrial purposes
TD201-500
spellingShingle reference evapotranspiration
multiple breakpoints
sensitivity analysis
vertical gradients
dominant climatic factor
mountainous area
Hydraulic engineering
TC1-978
Water supply for domestic and industrial purposes
TD201-500
Tingting Kang
Zeng Li
Yanchun Gao
Spatiotemporal Variations of Reference Evapotranspiration and Its Determining Climatic Factors in the Taihang Mountains, China
description Reference evapotranspiration (ETo) is an effective measure of atmospheric water demand of the land surface. In-depth investigations of the relationship between ETo and primary climatic factors can facilitate the adaptable agriculture and optimize water management, especially in the ecologically fragile Taihang Mountains (THM). This work assessed the spatiotemporal dynamics of ETo and its driving climatic factors from 1973 to 2016 in THM. Results showed: (1) Annual ETo slightly increased during 1973–2016; relative humidity (RH) decreased more slowly, the temperature increased more rapidly, and wind speed (WS) decreased more rapidly at higher elevation than those at lower elevations; (2) two breakpoints occurred in ETo series at 1990 and 1997, and an “evaporation paradox” existed in 1973–1990; (3) ETo at higher elevations had greater sensitivity to changes in RH and lower sensitivity to changes in Tmax and WS. Sensitivity of ETo to minimum air temperature (Tmin) at middle elevations was lowest among three elevation bands; (4) RH and sunshine duration (SD) were the dominant climatic factors of ETo for most periods and stations. This study helps us understand the impact of climate change on ETo in mountainous areas and confirms reference evapotranspiration in high-elevation areas is particularly sensitive to climate change.
format article
author Tingting Kang
Zeng Li
Yanchun Gao
author_facet Tingting Kang
Zeng Li
Yanchun Gao
author_sort Tingting Kang
title Spatiotemporal Variations of Reference Evapotranspiration and Its Determining Climatic Factors in the Taihang Mountains, China
title_short Spatiotemporal Variations of Reference Evapotranspiration and Its Determining Climatic Factors in the Taihang Mountains, China
title_full Spatiotemporal Variations of Reference Evapotranspiration and Its Determining Climatic Factors in the Taihang Mountains, China
title_fullStr Spatiotemporal Variations of Reference Evapotranspiration and Its Determining Climatic Factors in the Taihang Mountains, China
title_full_unstemmed Spatiotemporal Variations of Reference Evapotranspiration and Its Determining Climatic Factors in the Taihang Mountains, China
title_sort spatiotemporal variations of reference evapotranspiration and its determining climatic factors in the taihang mountains, china
publisher MDPI AG
publishDate 2021
url https://doaj.org/article/0b46699a01894a51a3104a25ff6243a1
work_keys_str_mv AT tingtingkang spatiotemporalvariationsofreferenceevapotranspirationanditsdeterminingclimaticfactorsinthetaihangmountainschina
AT zengli spatiotemporalvariationsofreferenceevapotranspirationanditsdeterminingclimaticfactorsinthetaihangmountainschina
AT yanchungao spatiotemporalvariationsofreferenceevapotranspirationanditsdeterminingclimaticfactorsinthetaihangmountainschina
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