2014
DOI: 10.1016/j.rse.2014.08.013
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Validation of Land Surface Temperature products derived from the Visible Infrared Imaging Radiometer Suite (VIIRS) using ground-based and heritage satellite measurements

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Cited by 127 publications
(104 citation statements)
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“…However, this is not an absolute validation unless one of the satellite products has been independently validated [21]. As the VIIRS is expected to replace MODIS in the future, the cross comparison to the MODIS LST will provide the evaluation of the VIIRS LST retrieval performance with respect to characterization of the differences, i.e., spatial pattern, systematic error budget, which may reflect the algorithm difference, limitations and error sources.…”
Section: Cross Satellite Comparison Methodsmentioning
confidence: 99%
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“…However, this is not an absolute validation unless one of the satellite products has been independently validated [21]. As the VIIRS is expected to replace MODIS in the future, the cross comparison to the MODIS LST will provide the evaluation of the VIIRS LST retrieval performance with respect to characterization of the differences, i.e., spatial pattern, systematic error budget, which may reflect the algorithm difference, limitations and error sources.…”
Section: Cross Satellite Comparison Methodsmentioning
confidence: 99%
“…The pyranometer is usually mounted on a 10 meter high tower in each SURFRAD site, facing downward to measure the surface upwelling radiation. The spatial representativeness is about 70 m × 70 m [21]. Observations from SURFRAD stations have been widely used for evaluating satellite-based estimates of surface radiation, for validating hydrology, weather prediction, climate models and satellite LST products from ASTER, GOES and MODIS [1,15,[30][31][32][33].…”
Section: Surfrad Ground Observationsmentioning
confidence: 99%
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“…However, a previous study indicated that assigning a fixed emissivity value to the barren soil may lead to an overestimation of the spectral emissivity values over very warm arid regions and generally results in an underestimation of the LST over these regions. Using maps of physically retrieved dynamic surface emissivities (like those from ASTER-TES, MODIS MOD11B1 or MOD21 products) as algorithm inputs may improve the inversion accuracy of the GSW algorithm [37,39] for barren surfaces. Hence, the ASTER emissivity dataset is used to calculate the band emissivities of the four evaluation sites.…”
Section: Calculations Of Lsementioning
confidence: 99%
“…Previous studies [37,39] indicated that the split-window algorithms generally underestimate the LST over very warm arid regions, especially barren surfaces. The barren surface emissivity values used in the split-window algorithm are constants and only depend on surface type.…”
Section: Introductionmentioning
confidence: 97%