2016
DOI: 10.3390/rs8120983
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The Modified SEBAL for Mapping Daily Spatial Evapotranspiration of South Korea Using Three Flux Towers and Terra MODIS Data

Abstract: Evapotranspiration (ET) is expected to increase by a considerable amount because of the impact of future temperature increase. Nowadays, the daily to seasonal ET maps can be used to provide information for a sustainable and adaptive watershed eco-environment. This study attempts to estimate the spatial ET of South Korea (99,900 km 2 ), located within the latitudes of 33 • 06 N to 43 • 01 N and the longitudes of 124 • 04 E to 131 • 05 E, on a daily basis. The satellite-based image-processing model Surface Energ… Show more

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Cited by 28 publications
(16 citation statements)
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“…Several methods have been developed to estimate ET from remotesensing data including empirical and statistical methods with remotely sensed vegetation indices [16][17][18], physical models that calculate ET as the residual of SEB using remotely sensed thermal infrared (IR) data [19][20][21][22][23][24][25], and other physical models such as the Penman-Monteith equations [26], the revised Resistance-Surface energy balance and the PenmanMonteith (RS-PM) equations [27][28][29] and Priestley-Taylor equations [30][31][32]. On a global or continental scales, the spatial ET is provided by the European Organization for the Exploitation of Meteorological Satellites (EUMETSAT) Satellite Application Facility (SAF) on Land Surface Analysis (LSA) and the National Aeronautics and Space Administration (NASA).…”
Section: Journal Of Sensorsmentioning
confidence: 99%
“…Several methods have been developed to estimate ET from remotesensing data including empirical and statistical methods with remotely sensed vegetation indices [16][17][18], physical models that calculate ET as the residual of SEB using remotely sensed thermal infrared (IR) data [19][20][21][22][23][24][25], and other physical models such as the Penman-Monteith equations [26], the revised Resistance-Surface energy balance and the PenmanMonteith (RS-PM) equations [27][28][29] and Priestley-Taylor equations [30][31][32]. On a global or continental scales, the spatial ET is provided by the European Organization for the Exploitation of Meteorological Satellites (EUMETSAT) Satellite Application Facility (SAF) on Land Surface Analysis (LSA) and the National Aeronautics and Space Administration (NASA).…”
Section: Journal Of Sensorsmentioning
confidence: 99%
“…However, there is still a need to refine the endmembers selection process, which will further improve the model accuracy since estimations are sensitive to changes in endmembers [55][56][57][58]. Regional applications of the SEBAL are usually based on local meteorological measurements [52,55,59,60], including wind speed ( ), relative humidity ( ), and shortwave incident radiation ( ). On the other hand, large-scale estimations can potentially benefit from the use of global, gridded meteorological variables (e.g., reanalysis methods) due to their global spatial coverage and long time-series [17,21,24,[61][62][63].…”
Section: Research Overviewmentioning
confidence: 99%
“…The instantaneous value can be used to calculate the daily value because the evaporative fraction tends to be constant during daytime hours, although the H and λE fluxes vary considerably [19,24]. The difference between the instantaneous evaporative fraction at satellite overpass and the evaporative fraction derived from the 24-h integrated energy balance is marginal and may be neglected [19,25,26].…”
Section: Methodsmentioning
confidence: 99%