2021
DOI: 10.1016/j.aej.2020.11.001
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Spatiotemporal assessment of actual evapotranspiration using satellite remote sensing technique in the Nile Delta, Egypt

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Cited by 16 publications
(9 citation statements)
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“…Due to these limitations, several remote sensing (RS)-based models and algorithms have been developed to quantify the ET a in rice, complementing the agrometeorological data observed on the ground and providing more detailed spatial information. Most of them are based on the surface energy balance, e.g., the Simplified Surface Energy Balance Index (S-SEBI) [18], Surface Energy Balance Algorithm for Land (SEBAL) [19], and Mapping Evapotranspiration at High Spatial Resolution with Internalized Calibration (METRIC) [20]; other models couple biophysical parameters and energy balance, e.g., the Breathing Earth System Simulator (BESS) [21], while others combine carbon and vapor fluxes through the response of the canopy conductance to the photosynthesis rate (PML-V2) [22], or integrate earth observations (i.e., the MODIS surface reflectance, albedo, and daily ground surface climate datasets) and numerical algorithms to calculate the ET a [23].…”
Section: Introductionmentioning
confidence: 99%
“…Due to these limitations, several remote sensing (RS)-based models and algorithms have been developed to quantify the ET a in rice, complementing the agrometeorological data observed on the ground and providing more detailed spatial information. Most of them are based on the surface energy balance, e.g., the Simplified Surface Energy Balance Index (S-SEBI) [18], Surface Energy Balance Algorithm for Land (SEBAL) [19], and Mapping Evapotranspiration at High Spatial Resolution with Internalized Calibration (METRIC) [20]; other models couple biophysical parameters and energy balance, e.g., the Breathing Earth System Simulator (BESS) [21], while others combine carbon and vapor fluxes through the response of the canopy conductance to the photosynthesis rate (PML-V2) [22], or integrate earth observations (i.e., the MODIS surface reflectance, albedo, and daily ground surface climate datasets) and numerical algorithms to calculate the ET a [23].…”
Section: Introductionmentioning
confidence: 99%
“…Access to reliable estimates of ET is important to many applications, including in the fields of climatology, meteorology, and agronomy [2]. For example, as a key indicator of crop growth, ET can be used to calculate the amount of water that is consumed by crops, so it holds vast potential for agricultural irrigation [3][4][5][6]. Climate change can cause changes in temperature and wind speed, which will change the processes of the water cycle and energy balance.…”
Section: Introductionmentioning
confidence: 99%
“…The disadvantage of this method is that new errors will be generated on the LST during the resampling or downscaling process, which will result in issues with the LE estimates; (3) an area-weighting method, which uses high-resolution land cover classification data to decompose the mixed pixels of the large-resolution data, and calculates the roughness length and H based on subpixel landscapes, then weighs the H of each sub-pixel according to the area ratio to obtain the H of the entire mixed pixel. Eventually, LE is corrected through correcting H. This method can improve the accuracy of estimating LE to a certain extent but does not fundamentally solve the heterogeneity of the land surface [43,44]; (4) an evaporative fraction and area fraction (EFAF) method. Li et al first applied the EFAF method to correct the deviation of the LE with a spatial resolution of 300 m and proved its feasibility [45].…”
Section: Introductionmentioning
confidence: 99%
“…Its registered accuracies of 85% on a farm-scale while more than 95% accuracy was recorded on a regional scale (Seneviratne et al 2006). Fawzy et al (2021) used Landsat satellite data with the SEBAL algorithm to study daily evapotranspiration in the Nile Delta, Egypt, and reported that the SEBAL method estimated the transpiration evaporation of the region with acceptable accuracy. The purpose of this study was to compute the actual evapotranspiration (ET) from SEBAL using Landsat 8 images in the the lower bhavani basin, Tamil Nadu.…”
Section: Introductionmentioning
confidence: 99%