2022
DOI: 10.1016/j.rse.2021.112774
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Determination of global land surface temperature using data from only five selected thermal infrared channels: Method extension and accuracy assessment

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Cited by 24 publications
(7 citation statements)
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“…The formula L sen is the brightness of the thermal radiation received by the sensor in units [W/(m 2 sr μm)]; T sen represents the brightness temperature in K; λ is the effective wavelength in μm; ε is the surface specific emissivity; δ is the surface specific emissivity; C 1 = l.19104 W × 108 W/(m 2 ·sr·m); C 2 = 1.43877 × 104 mK; In the surface temperature inversion formula ψ 1 , ψ 2 , and ψ 3 are intermediate variables that are cubic trinomials concerning atmospheric water vapor content ω, and the function expression is as follows (Zheng et al, 2022):…”
Section: Methodsmentioning
confidence: 99%
See 1 more Smart Citation
“…The formula L sen is the brightness of the thermal radiation received by the sensor in units [W/(m 2 sr μm)]; T sen represents the brightness temperature in K; λ is the effective wavelength in μm; ε is the surface specific emissivity; δ is the surface specific emissivity; C 1 = l.19104 W × 108 W/(m 2 ·sr·m); C 2 = 1.43877 × 104 mK; In the surface temperature inversion formula ψ 1 , ψ 2 , and ψ 3 are intermediate variables that are cubic trinomials concerning atmospheric water vapor content ω, and the function expression is as follows (Zheng et al, 2022):…”
Section: Methodsmentioning
confidence: 99%
“…The surface temperature is first inverted using a single-channel algorithm and thermal infrared to bring in the thermal emissivity of the surface combined with the atmospheric water vapor content to be able to invert the surface air temperature. The equations are as follows (Zheng et al, 2022):…”
Section: Methodsmentioning
confidence: 99%
“…Therefore, the experiments were conducted in relatively dry atmospheric conditions in this paper. The use of more robust LST estimation methods, such as the hybrid algorithm that requires no additional input [42][43][44], will be applied to enable the algorithms to be suitable to a wider range of atmospheric conditions. Moreover, the empirical relationship between solar radiance and CWV has been summarized in previous studies [45].…”
Section: Future Improvements Of the Proposed Methodsmentioning
confidence: 99%
“…Land surface temperature (LST) is one of the key parameters for studying processes in land surface systems at regional and global scales, enabling monitoring of the spatial and temporal variability in the energy balance state at the surface [ 1 , 2 , 3 , 4 ]. Satellite thermal infrared remote sensing is an effective means of obtaining LST [ 5 , 6 , 7 , 8 ]. With the rapid development of remote sensing technology and inversion algorithms, LST data obtained by thermal infrared remote sensing inversion algorithms are widely used in various fields, such as evapotranspiration and soil moisture estimation [ 9 ], urban heat island studies [ 10 , 11 , 12 , 13 ], disaster monitoring [ 14 ], and environmental monitoring [ 15 ].…”
Section: Introductionmentioning
confidence: 99%