1992
DOI: 10.1016/0034-4257(92)90096-3
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A comparison of techniques for extracting emissivity information from thermal infrared data for geologic studies

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Cited by 223 publications
(101 citation statements)
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“…It acquires day and night multi-spectral infrared images at 100 meters per pixel spatial resolution, and one-band visible images at 18 meters per pixel (Christensen et al, 2004). Infrared imagery allows physical surface characteristics to be better distinguished than images taken at visible light wavelengths (Hook, Gabell, Green, & Kealy, 1992;Kahle, Gillespie, & Goetz, 1976;Watson, 1975). THEMIS has an extensive coverage of Mars, which is almost complete in the infrared (≈96% for daytime and ≈82% nighttime coverage, Figure 2).…”
Section: Thermal Emision Imaging System (Themis)mentioning
confidence: 99%
“…It acquires day and night multi-spectral infrared images at 100 meters per pixel spatial resolution, and one-band visible images at 18 meters per pixel (Christensen et al, 2004). Infrared imagery allows physical surface characteristics to be better distinguished than images taken at visible light wavelengths (Hook, Gabell, Green, & Kealy, 1992;Kahle, Gillespie, & Goetz, 1976;Watson, 1975). THEMIS has an extensive coverage of Mars, which is almost complete in the infrared (≈96% for daytime and ≈82% nighttime coverage, Figure 2).…”
Section: Thermal Emision Imaging System (Themis)mentioning
confidence: 99%
“…The visible through SWIR bands (1-25) were processed to surface reflectance, the MIR bands (26)(27)(28)(29)(30)(31)(32)(33)(34)(35)(36)(37)(38)(39)(40) were not atmospherically corrected and the thermal bands (41)(42)(43)(44)(45)(46)(47)(48)(49)(50) were atmospherically corrected to surface radiance. The surface radiance of the thermal bands was then separated into surface temperature (T s ) and surface emissivity ( ) using the emissivity normalization method [54]. is defined as the ratio of the actual emitted radiance to the radiance emitted from a blackbody at the same thermodynamic temperature [55,56].…”
Section: Master Imagery and Preprocessingmentioning
confidence: 99%
“…The algorithms to separate temperature and emissivity are generally complex and problematic because of the nonlinearity in the relative contributions of temperature and emissivity effects [12][13][14]. The extracted emissivity products have a relatively high uncertainty and low contrast, which may subdue spectral features and limit the discrimination accuracy [15,16]. A rock index is generally sensitive to a specific rock or mineral and is not enough to identify other rocks [4,6].…”
Section: Introductionmentioning
confidence: 99%