Temporal variations of reference evapotranspiration and its sensitivity to meteorological factors in Heihe River Basin, China

On the basis of daily meteorological data from 15 meteorological stations in the Heihe River Basin (HRB) during the period from 1959 to 2012, long-term trends of reference evapotranspiration (ET0) and key meteorological factors that affect ET0 were analyzed using the Mann-Kendall test. The evaporati...

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Main Authors: Jie Zhao, Zong-xue Xu, De-peng Zuo, Xu-ming Wang
Format: Article
Language:English
Published: Elsevier 2015-01-01
Series:Water Science and Engineering
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S1674237015000058
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spelling doaj-6a55d2bf0ee249628547ff9ada84f19d2020-11-24T22:51:21ZengElsevierWater Science and Engineering1674-23702015-01-01811810.1016/j.wse.2015.01.004Temporal variations of reference evapotranspiration and its sensitivity to meteorological factors in Heihe River Basin, ChinaJie ZhaoZong-xue XuDe-peng ZuoXu-ming WangOn the basis of daily meteorological data from 15 meteorological stations in the Heihe River Basin (HRB) during the period from 1959 to 2012, long-term trends of reference evapotranspiration (ET0) and key meteorological factors that affect ET0 were analyzed using the Mann-Kendall test. The evaporation paradox was also investigated at 15 meteorological stations. In order to explore the contribution of key meteorological factors to the temporal variation of ET0, a sensitivity coefficient method was employed in this study. The results show that: (1) mean annual air temperature significantly increased at all 15 meteorological stations, while the mean annual ET0 decreased at most of sites; (2) the evaporation paradox did exist in the HRB, while the evaporation paradox was not continuous in space and time; and (3) relative humidity was the most sensitive meteorological factor with regard to the temporal variation of ET0 in the HRB, followed by wind speed, air temperature, and solar radiation. Air temperature and solar radiation contributed most to the temporal variation of ET0 in the upper reaches; solar radiation and wind speed were the determining factors for the temporal variation of ET0 in the middle-lower reaches.http://www.sciencedirect.com/science/article/pii/S1674237015000058Reference evapotranspirationEvaporation paradoxMeteorological factorHeihe River Basin
collection DOAJ
language English
format Article
sources DOAJ
author Jie Zhao
Zong-xue Xu
De-peng Zuo
Xu-ming Wang
spellingShingle Jie Zhao
Zong-xue Xu
De-peng Zuo
Xu-ming Wang
Temporal variations of reference evapotranspiration and its sensitivity to meteorological factors in Heihe River Basin, China
Water Science and Engineering
Reference evapotranspiration
Evaporation paradox
Meteorological factor
Heihe River Basin
author_facet Jie Zhao
Zong-xue Xu
De-peng Zuo
Xu-ming Wang
author_sort Jie Zhao
title Temporal variations of reference evapotranspiration and its sensitivity to meteorological factors in Heihe River Basin, China
title_short Temporal variations of reference evapotranspiration and its sensitivity to meteorological factors in Heihe River Basin, China
title_full Temporal variations of reference evapotranspiration and its sensitivity to meteorological factors in Heihe River Basin, China
title_fullStr Temporal variations of reference evapotranspiration and its sensitivity to meteorological factors in Heihe River Basin, China
title_full_unstemmed Temporal variations of reference evapotranspiration and its sensitivity to meteorological factors in Heihe River Basin, China
title_sort temporal variations of reference evapotranspiration and its sensitivity to meteorological factors in heihe river basin, china
publisher Elsevier
series Water Science and Engineering
issn 1674-2370
publishDate 2015-01-01
description On the basis of daily meteorological data from 15 meteorological stations in the Heihe River Basin (HRB) during the period from 1959 to 2012, long-term trends of reference evapotranspiration (ET0) and key meteorological factors that affect ET0 were analyzed using the Mann-Kendall test. The evaporation paradox was also investigated at 15 meteorological stations. In order to explore the contribution of key meteorological factors to the temporal variation of ET0, a sensitivity coefficient method was employed in this study. The results show that: (1) mean annual air temperature significantly increased at all 15 meteorological stations, while the mean annual ET0 decreased at most of sites; (2) the evaporation paradox did exist in the HRB, while the evaporation paradox was not continuous in space and time; and (3) relative humidity was the most sensitive meteorological factor with regard to the temporal variation of ET0 in the HRB, followed by wind speed, air temperature, and solar radiation. Air temperature and solar radiation contributed most to the temporal variation of ET0 in the upper reaches; solar radiation and wind speed were the determining factors for the temporal variation of ET0 in the middle-lower reaches.
topic Reference evapotranspiration
Evaporation paradox
Meteorological factor
Heihe River Basin
url http://www.sciencedirect.com/science/article/pii/S1674237015000058
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AT zongxuexu temporalvariationsofreferenceevapotranspirationanditssensitivitytometeorologicalfactorsinheiheriverbasinchina
AT depengzuo temporalvariationsofreferenceevapotranspirationanditssensitivitytometeorologicalfactorsinheiheriverbasinchina
AT xumingwang temporalvariationsofreferenceevapotranspirationanditssensitivitytometeorologicalfactorsinheiheriverbasinchina
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