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• W2921189400 endingPage "4090" @default.
• W2921189400 startingPage "4072" @default.
• W2921189400 abstract "Accurate terrestrial evapotranspiration (ET) estimation and understanding the causes of ET variation are essential for water resource management and irrigation planning. In this research, the complementary relationship (CR) between actual evapotranspiration (ET a ) and potential evapotranspiration (ET p ) was evaluated. An Advection–Aridity (AA) model was calibrated and validated using eddy covariance measurements. The spatiotemporal variations of ET a , ET p and associated meteorological variables were examined through Mann–Kendall (MK) testing and Theil–Sen's estimator, using daily weather data from 137 meteorological stations in Huai River basin (HRB) during 1961–2014. Moreover, the influences of meteorological factors on ET a and ET p were quantified by the differential equation method. The results indicate that CR theory is applicable in the HRB and the calibrated AA model can simulate the ET a well. ET a exhibited a significant increasing trend before 1990 and then decreased significantly. However, ET p decreased significantly before 1990 and then declined slightly. During 1961–1990, except for significant increasing relative humidity (RH), other meteorological variables exhibited decreasing trends. The aerodynamic component dominated ET a and ET p trends in general. The wind speed at 2‐m height ( u 2 ) dominated ET a trends except for summer and growing season and ET p trends except for summer, when the dominant factor is net radiation ( R n ). During 1991–2014, mean temperature ( T a ) and RH showed distinct increasing and decreasing trends, respectively, whereas significant decline in u 2 palpably slowed. The absolute value of the radiative component was larger than that of the aerodynamic one. The dominant factor of ET a trends shifted from u 2 to RH in spring and to R n in autumn, winter and annual timescales. Moreover, the dominant factor of ET p trends changed from u 2 to RH in spring, winter and annual timescales and to R n in growing season and autumn. R n always played a pivotal role in both ET a and ET p trends in summer." @default.
• W2921189400 created "2019-03-22" @default.
• W2921189400 creator A5037595706 @default.
• W2921189400 creator A5038855458 @default.
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• W2921189400 creator A5076195621 @default.
• W2921189400 creator A5077498658 @default.
• W2921189400 date "2019-04-03" @default.
• W2921189400 modified "2023-10-17" @default.
• W2921189400 title "Attribution analysis of actual and potential evapotranspiration changes based on the complementary relationship theory in the Huai River basin of eastern China" @default.
• W2921189400 cites W1531049992 @default.
• W2921189400 cites W1532996006 @default.
• W2921189400 cites W1534840979 @default.
• W2921189400 cites W1541152976 @default.
• W2921189400 cites W1634416795 @default.
• W2921189400 cites W1665103756 @default.
• W2921189400 cites W1756015726 @default.
• W2921189400 cites W1841159879 @default.
• W2921189400 cites W1912201981 @default.
• W2921189400 cites W1969974566 @default.
• W2921189400 cites W1971589869 @default.
• W2921189400 cites W1974634892 @default.
• W2921189400 cites W1978622845 @default.
• W2921189400 cites W1979723077 @default.
• W2921189400 cites W1981446211 @default.
• W2921189400 cites W1985478807 @default.
• W2921189400 cites W1989632257 @default.
• W2921189400 cites W1992846746 @default.
• W2921189400 cites W1993525836 @default.
• W2921189400 cites W1996706396 @default.
• W2921189400 cites W1998600947 @default.
• W2921189400 cites W2003868148 @default.
• W2921189400 cites W2005718628 @default.
• W2921189400 cites W2006768023 @default.
• W2921189400 cites W2013928862 @default.
• W2921189400 cites W2016236181 @default.
• W2921189400 cites W2018764772 @default.
• W2921189400 cites W2025422755 @default.
• W2921189400 cites W2030539462 @default.
• W2921189400 cites W2038180059 @default.
• W2921189400 cites W2041931938 @default.
• W2921189400 cites W2042751779 @default.
• W2921189400 cites W2055315489 @default.
• W2921189400 cites W2060923748 @default.
• W2921189400 cites W2061153033 @default.
• W2921189400 cites W2061260773 @default.
• W2921189400 cites W2063259011 @default.
• W2921189400 cites W2067973431 @default.
• W2921189400 cites W2079349192 @default.
• W2921189400 cites W2081591623 @default.
• W2921189400 cites W2082934097 @default.
• W2921189400 cites W2083412663 @default.
• W2921189400 cites W2084637553 @default.
• W2921189400 cites W2084944700 @default.
• W2921189400 cites W2087169535 @default.
• W2921189400 cites W2087864093 @default.
• W2921189400 cites W2088135986 @default.
• W2921189400 cites W2096440910 @default.
• W2921189400 cites W2106235239 @default.
• W2921189400 cites W2115607306 @default.
• W2921189400 cites W2120328133 @default.
• W2921189400 cites W2126495193 @default.
• W2921189400 cites W2129161539 @default.
• W2921189400 cites W2131517559 @default.
• W2921189400 cites W2132237213 @default.
• W2921189400 cites W2135518940 @default.
• W2921189400 cites W2144378718 @default.
• W2921189400 cites W2146282881 @default.
• W2921189400 cites W2146937058 @default.
• W2921189400 cites W2151834066 @default.
• W2921189400 cites W2156564013 @default.
• W2921189400 cites W2157896052 @default.
• W2921189400 cites W2158374691 @default.
• W2921189400 cites W2158811585 @default.
• W2921189400 cites W2164516565 @default.
• W2921189400 cites W2165386375 @default.
• W2921189400 cites W2166186402 @default.
• W2921189400 cites W2167453193 @default.
• W2921189400 cites W2172396214 @default.
• W2921189400 cites W2174289972 @default.
• W2921189400 cites W2176244925 @default.
• W2921189400 cites W2236687958 @default.
• W2921189400 cites W2285422781 @default.
• W2921189400 cites W2318680928 @default.
• W2921189400 cites W2330638704 @default.
• W2921189400 cites W2471545429 @default.
• W2921189400 cites W2499013147 @default.
• W2921189400 cites W2512881071 @default.
• W2921189400 cites W2527066115 @default.
• W2921189400 cites W2549557007 @default.
• W2921189400 cites W2604569851 @default.
• W2921189400 cites W2731682763 @default.
• W2921189400 cites W2733867881 @default.
• W2921189400 cites W2772886797 @default.
• W2921189400 cites W2775579480 @default.
• W2921189400 cites W2776240795 @default.
• W2921189400 cites W2793860551 @default.
• W2921189400 cites W2794421688 @default.

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