Evapotranspiration Estimation Using Remote Sensing Technology Based on a SEBAL Model in the Upper Reaches of the Huaihe River Basin

Understanding the spatial and temporal variations of evapotranspiration (<i>ET</i>) is vital for water resources planning and management and drought monitoring. The development of a satellite remote sensing technique is described to provide insight into the estimation of <i>ET</...

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Main Authors: Linshan Tan, Kaiyuan Zheng, Qiangqiang Zhao, Yanjuan Wu
Format: Article
Language:English
Published: MDPI AG 2021-11-01
Series:Atmosphere
Subjects:
Online Access:https://www.mdpi.com/2073-4433/12/12/1599
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author Linshan Tan
Kaiyuan Zheng
Qiangqiang Zhao
Yanjuan Wu
author_facet Linshan Tan
Kaiyuan Zheng
Qiangqiang Zhao
Yanjuan Wu
author_sort Linshan Tan
collection DOAJ
description Understanding the spatial and temporal variations of evapotranspiration (<i>ET</i>) is vital for water resources planning and management and drought monitoring. The development of a satellite remote sensing technique is described to provide insight into the estimation of <i>ET</i> at a regional scale. In this study, the Surface Energy Balance Algorithm for Land (SEBAL) was used to calculate the actual <i>ET</i> on a daily scale from Landsat-8 data and daily ground-based meteorological data in the upper reaches of Huaihe River on 20 November 2013, 16 April 2015 and 23 March 2018. In order to evaluate the performance of the SEBAL model, the daily SEBAL <i>ET</i> (<i>ET</i><sub>SEBAL</sub>) was compared against the daily reference <i>ET</i> (<i>ET</i><sub>0</sub>) from four theoretical methods: the Penman-Monteith (P-M), Irmak-Allen (I-A), the Turc, and Jensen-Haise (J-H) method, the <i>ET</i><sub>MOD16</sub> product from the MODerate Resolution Imaging Spectrometer (MOD16) and the <i>ET</i><sub>VIC</sub> from Variable Infiltration Capacity Model (VIC). A linear regression equation and statistical indices were used to model performance evaluation. The results showed that the daily <i>ET</i><sub>SEBAL</sub> correlated very well with the <i>ET</i><sub>0</sub>, <i>ET</i><sub>MOD16</sub>, and <i>ET</i><sub>VIC</sub>, and bias between the <i>ET</i><sub>SEBAL</sub> with them was less than 1.5%. In general, the SEBAL model could provide good estimations in daily <i>ET</i> over the study region. In addition, the spatial-temporal distribution of <i>ET</i><sub>SEBAL</sub> was explored. The variation of <i>ET</i><sub>SEBAL</sub> was significant in seasons with high values during the growth period of vegetation in March and April and low values in November. Spatially, the daily <i>ET</i><sub>SEBAL</sub> values in the mountain area were much higher than those in the plain areas over the study region. The variability of <i>ET</i><sub>SEBAL</sub> in this study area was positively correlated with elevation and negatively correlated with surface reflectance, which implies that elevation and surface reflectance are the important factors for predicting <i>ET</i> in this study area.
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spelling doaj.art-6d7c20bd1622428fa73918a25d13c15a2023-11-23T03:46:04ZengMDPI AGAtmosphere2073-44332021-11-011212159910.3390/atmos12121599Evapotranspiration Estimation Using Remote Sensing Technology Based on a SEBAL Model in the Upper Reaches of the Huaihe River BasinLinshan Tan0Kaiyuan Zheng1Qiangqiang Zhao2Yanjuan Wu3Department of Geography and Spatial Information Techniques, Ningbo University, Ningbo 315211, ChinaNingbo Universities Collaborative Innovation Center for Land and Marine Spatial Utilization and Governance Research, Ningbo University, Ningbo 315211, ChinaDepartment of Geography and Spatial Information Techniques, Ningbo University, Ningbo 315211, ChinaDepartment of Geography and Spatial Information Techniques, Ningbo University, Ningbo 315211, ChinaUnderstanding the spatial and temporal variations of evapotranspiration (<i>ET</i>) is vital for water resources planning and management and drought monitoring. The development of a satellite remote sensing technique is described to provide insight into the estimation of <i>ET</i> at a regional scale. In this study, the Surface Energy Balance Algorithm for Land (SEBAL) was used to calculate the actual <i>ET</i> on a daily scale from Landsat-8 data and daily ground-based meteorological data in the upper reaches of Huaihe River on 20 November 2013, 16 April 2015 and 23 March 2018. In order to evaluate the performance of the SEBAL model, the daily SEBAL <i>ET</i> (<i>ET</i><sub>SEBAL</sub>) was compared against the daily reference <i>ET</i> (<i>ET</i><sub>0</sub>) from four theoretical methods: the Penman-Monteith (P-M), Irmak-Allen (I-A), the Turc, and Jensen-Haise (J-H) method, the <i>ET</i><sub>MOD16</sub> product from the MODerate Resolution Imaging Spectrometer (MOD16) and the <i>ET</i><sub>VIC</sub> from Variable Infiltration Capacity Model (VIC). A linear regression equation and statistical indices were used to model performance evaluation. The results showed that the daily <i>ET</i><sub>SEBAL</sub> correlated very well with the <i>ET</i><sub>0</sub>, <i>ET</i><sub>MOD16</sub>, and <i>ET</i><sub>VIC</sub>, and bias between the <i>ET</i><sub>SEBAL</sub> with them was less than 1.5%. In general, the SEBAL model could provide good estimations in daily <i>ET</i> over the study region. In addition, the spatial-temporal distribution of <i>ET</i><sub>SEBAL</sub> was explored. The variation of <i>ET</i><sub>SEBAL</sub> was significant in seasons with high values during the growth period of vegetation in March and April and low values in November. Spatially, the daily <i>ET</i><sub>SEBAL</sub> values in the mountain area were much higher than those in the plain areas over the study region. The variability of <i>ET</i><sub>SEBAL</sub> in this study area was positively correlated with elevation and negatively correlated with surface reflectance, which implies that elevation and surface reflectance are the important factors for predicting <i>ET</i> in this study area.https://www.mdpi.com/2073-4433/12/12/1599evapotranspirationHuaihe River BasinSEBAL modelspatial distribution
spellingShingle Linshan Tan
Kaiyuan Zheng
Qiangqiang Zhao
Yanjuan Wu
Evapotranspiration Estimation Using Remote Sensing Technology Based on a SEBAL Model in the Upper Reaches of the Huaihe River Basin
Atmosphere
evapotranspiration
Huaihe River Basin
SEBAL model
spatial distribution
title Evapotranspiration Estimation Using Remote Sensing Technology Based on a SEBAL Model in the Upper Reaches of the Huaihe River Basin
title_full Evapotranspiration Estimation Using Remote Sensing Technology Based on a SEBAL Model in the Upper Reaches of the Huaihe River Basin
title_fullStr Evapotranspiration Estimation Using Remote Sensing Technology Based on a SEBAL Model in the Upper Reaches of the Huaihe River Basin
title_full_unstemmed Evapotranspiration Estimation Using Remote Sensing Technology Based on a SEBAL Model in the Upper Reaches of the Huaihe River Basin
title_short Evapotranspiration Estimation Using Remote Sensing Technology Based on a SEBAL Model in the Upper Reaches of the Huaihe River Basin
title_sort evapotranspiration estimation using remote sensing technology based on a sebal model in the upper reaches of the huaihe river basin
topic evapotranspiration
Huaihe River Basin
SEBAL model
spatial distribution
url https://www.mdpi.com/2073-4433/12/12/1599
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AT kaiyuanzheng evapotranspirationestimationusingremotesensingtechnologybasedonasebalmodelintheupperreachesofthehuaiheriverbasin
AT qiangqiangzhao evapotranspirationestimationusingremotesensingtechnologybasedonasebalmodelintheupperreachesofthehuaiheriverbasin
AT yanjuanwu evapotranspirationestimationusingremotesensingtechnologybasedonasebalmodelintheupperreachesofthehuaiheriverbasin