2016
DOI: 10.1016/j.isprsjprs.2016.01.007
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Effect of emissivity uncertainty on surface temperature retrieval over urban areas: Investigations based on spectral libraries

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Cited by 50 publications
(29 citation statements)
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“…The spectra in ASTER Spectral Library Version 2.0 are available from http://speclib.jpl.nasa.gov. However, as discussed previously (Chen et al, 2016), difference in wavelength range and spectral resolution between the SRFs of the channels and the spectra may result in bias in channel reflectance calculation (see Eq.…”
Section: Spectra Datamentioning
confidence: 99%
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“…The spectra in ASTER Spectral Library Version 2.0 are available from http://speclib.jpl.nasa.gov. However, as discussed previously (Chen et al, 2016), difference in wavelength range and spectral resolution between the SRFs of the channels and the spectra may result in bias in channel reflectance calculation (see Eq.…”
Section: Spectra Datamentioning
confidence: 99%
“…Accordingly, a collection of 897 spectra obtained from ASTER Spectral Library Version 2.0 was used in further investigations. An interpolation procedure (Chen et al, 2016) was used to tackle the difference in spectral resolution. Additionally, a collection of spectra from Hyperion data archives was selected (Claverie et al, 2017).…”
Section: Spectra Datamentioning
confidence: 99%
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“…Emissivity is a critical variable for the LST estimation, since a small uncertainty in the emissivity (1%) can lead to large errors in the LST (up to 1 K) depending on the setting of the sensor, the climatological conditions and geographical setting of the area [41,42]. In this study, three different sources of emissivity are used: ASTER and MODIS emissivity that are available in the GEE catalogue and NDVI-based emissivity estimated from Landsat red and near-infrared data.…”
Section: Emissivitymentioning
confidence: 99%
“…Even if in most investigations the importance and potential impacts of urban surface emissivity were ignored, often due to data unavailability, for accurate quantitative temperature analysis they must necessarily be considered. 13 Several methods can be followed to separate the effects of both surface emissivity and temperature on the radiance at ground level; however, even with multi-spectral sensors with N thermal channels available, the system composed of N radiative transfer equations (one for each channel) remains mathematically unsolvable, because there will always be N + 1 unknowns, corresponding to the N emissivities in each wavelength and the surface temperature. 11 On the basis of the number of thermal infrared channels available, the methods to derive the land surface temperature were categorized in four main groups: 14, 15 single channel methods, double channel (or split-window) methods, two angle methods and other methods, developed for sensors operating in more than two infrared channels or based on different techniques.…”
Section: Methodsmentioning
confidence: 99%