Estimating Calibration Variability in Evapotranspiration Derived from a Satellite-Based Energy Balance Model

Computing evapotranspiration (ET) with satellite-based energy balance models such as METRIC (Mapping EvapoTranspiration at high Resolution with Internalized Calibration) requires internal calibration of sensible heat flux using anchor pixels (“hot„ and “cold„...

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Main Authors: Sulochan Dhungel, Michael E. Barber
Format: Article
Language:English
Published: MDPI AG 2018-10-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/10/11/1695
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spelling doaj-8e8e1c53b54e44b29df8c74cc574b6cc2020-11-24T21:51:16ZengMDPI AGRemote Sensing2072-42922018-10-011011169510.3390/rs10111695rs10111695Estimating Calibration Variability in Evapotranspiration Derived from a Satellite-Based Energy Balance ModelSulochan Dhungel0Michael E. Barber1Department of Civil and Environmental Engineering, University of Utah, 110 S. Central Campus Drive, Salt Lake City, UT 84112, USADepartment of Civil and Environmental Engineering, University of Utah, 110 S. Central Campus Drive, Salt Lake City, UT 84112, USAComputing evapotranspiration (ET) with satellite-based energy balance models such as METRIC (Mapping EvapoTranspiration at high Resolution with Internalized Calibration) requires internal calibration of sensible heat flux using anchor pixels (&#8220;hot&#8222; and &#8220;cold&#8222; pixels). Despite the development of automated anchor pixel selection methods that classify a pool of candidate pixels using the amount of vegetation (normalized difference vegetation index, NDVI) and surface temperature (<i>T<sub>s</sub></i>), final pixel selection still relies heavily on operator experience. Yet, differences in final ET estimates resulting from subjectivity in selecting the final &#8220;hot&#8222; and &#8220;cold&#8222; pixel pair (from within the candidate pixel pool) have not yet been investigated. This is likely because surface properties of these candidate pixels, as quantified by NDVI and surface temperature, are generally assumed to have low variability that can be attributed to random noise. In this study, we test the assumption of low variability by first applying an automated calibration pixel selection process to 42 nearly cloud-free Landsat images of the San Joaquin area in California taken between 2013 and 2015. We then compute <i>T<sub>s</sub></i> (vertical near-surface temperature differences) vs. <i>T<sub>s</sub></i> relationships at all pixels that could potentially be used for model calibration in order to explore ET variance between the results from multiple calibration schemes where NDVI and <i>T<sub>s</sub></i> variability is intrinsically negligible. Our results show significant variability in ET (ranging from 5% to 20%) and a high&#8212;and statistically consistent&#8212;variability in <i>dT</i> values, indicating that there are additional surface properties affecting the calibration process not captured when using only NDVI and <i>T<sub>s</sub></i>. Our findings further highlight the potential for calibration improvements by showing that the <i>dT</i> vs. <i>T<sub>s</sub></i> calibration relationship between the cold anchor pixel (with lowest <i>dT</i>) and the hot anchor pixel (with highest <i>dT</i>) consistently provides the best daily ET estimates. This approach of quantifying ET variability based on candidate pixel selection and the accompanying results illustrate an approach to quantify the biases inadvertently introduced by user subjectivity and can be used to inform improvements on model usability and performance.https://www.mdpi.com/2072-4292/10/11/1695remote sensingsurface energy balance modelcalibrationMETRICGoogle Earth Engine
collection DOAJ
language English
format Article
sources DOAJ
author Sulochan Dhungel
Michael E. Barber
spellingShingle Sulochan Dhungel
Michael E. Barber
Estimating Calibration Variability in Evapotranspiration Derived from a Satellite-Based Energy Balance Model
Remote Sensing
remote sensing
surface energy balance model
calibration
METRIC
Google Earth Engine
author_facet Sulochan Dhungel
Michael E. Barber
author_sort Sulochan Dhungel
title Estimating Calibration Variability in Evapotranspiration Derived from a Satellite-Based Energy Balance Model
title_short Estimating Calibration Variability in Evapotranspiration Derived from a Satellite-Based Energy Balance Model
title_full Estimating Calibration Variability in Evapotranspiration Derived from a Satellite-Based Energy Balance Model
title_fullStr Estimating Calibration Variability in Evapotranspiration Derived from a Satellite-Based Energy Balance Model
title_full_unstemmed Estimating Calibration Variability in Evapotranspiration Derived from a Satellite-Based Energy Balance Model
title_sort estimating calibration variability in evapotranspiration derived from a satellite-based energy balance model
publisher MDPI AG
series Remote Sensing
issn 2072-4292
publishDate 2018-10-01
description Computing evapotranspiration (ET) with satellite-based energy balance models such as METRIC (Mapping EvapoTranspiration at high Resolution with Internalized Calibration) requires internal calibration of sensible heat flux using anchor pixels (&#8220;hot&#8222; and &#8220;cold&#8222; pixels). Despite the development of automated anchor pixel selection methods that classify a pool of candidate pixels using the amount of vegetation (normalized difference vegetation index, NDVI) and surface temperature (<i>T<sub>s</sub></i>), final pixel selection still relies heavily on operator experience. Yet, differences in final ET estimates resulting from subjectivity in selecting the final &#8220;hot&#8222; and &#8220;cold&#8222; pixel pair (from within the candidate pixel pool) have not yet been investigated. This is likely because surface properties of these candidate pixels, as quantified by NDVI and surface temperature, are generally assumed to have low variability that can be attributed to random noise. In this study, we test the assumption of low variability by first applying an automated calibration pixel selection process to 42 nearly cloud-free Landsat images of the San Joaquin area in California taken between 2013 and 2015. We then compute <i>T<sub>s</sub></i> (vertical near-surface temperature differences) vs. <i>T<sub>s</sub></i> relationships at all pixels that could potentially be used for model calibration in order to explore ET variance between the results from multiple calibration schemes where NDVI and <i>T<sub>s</sub></i> variability is intrinsically negligible. Our results show significant variability in ET (ranging from 5% to 20%) and a high&#8212;and statistically consistent&#8212;variability in <i>dT</i> values, indicating that there are additional surface properties affecting the calibration process not captured when using only NDVI and <i>T<sub>s</sub></i>. Our findings further highlight the potential for calibration improvements by showing that the <i>dT</i> vs. <i>T<sub>s</sub></i> calibration relationship between the cold anchor pixel (with lowest <i>dT</i>) and the hot anchor pixel (with highest <i>dT</i>) consistently provides the best daily ET estimates. This approach of quantifying ET variability based on candidate pixel selection and the accompanying results illustrate an approach to quantify the biases inadvertently introduced by user subjectivity and can be used to inform improvements on model usability and performance.
topic remote sensing
surface energy balance model
calibration
METRIC
Google Earth Engine
url https://www.mdpi.com/2072-4292/10/11/1695
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AT michaelebarber estimatingcalibrationvariabilityinevapotranspirationderivedfromasatellitebasedenergybalancemodel
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