A Physically Constrained Calibration Database for Land Surface Temperature Using Infrared Retrieval Algorithms
Land surface temperature (LST) is routinely retrieved from remote sensing instruments using semi-empirical relationships between top of atmosphere (TOA) radiances and LST, using ancillary data such as total column water vapor or emissivity. These algorithms are calibrated using a set of forward radi...
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doaj-7a496a26a13e4c6dab0cad1795c43fd32020-11-24T20:51:24ZengMDPI AGRemote Sensing2072-42922016-09-0181080810.3390/rs8100808rs8100808A Physically Constrained Calibration Database for Land Surface Temperature Using Infrared Retrieval AlgorithmsJoão P. A. Martins0Isabel F. Trigo1Virgílio A. Bento2Carlos da Camara3Instituto Português do Mar e da Atmosfera, 1749-077 Lisbon, PortugalInstituto Português do Mar e da Atmosfera, 1749-077 Lisbon, PortugalInstituto Dom Luiz, University of Lisbon, IDL, Campo Grande, Ed C1, 1749-016 Lisbon, PortugalInstituto Dom Luiz, University of Lisbon, IDL, Campo Grande, Ed C1, 1749-016 Lisbon, PortugalLand surface temperature (LST) is routinely retrieved from remote sensing instruments using semi-empirical relationships between top of atmosphere (TOA) radiances and LST, using ancillary data such as total column water vapor or emissivity. These algorithms are calibrated using a set of forward radiative transfer simulations that return the TOA radiances given the LST and the thermodynamic profiles. The simulations are done in order to cover a wide range of surface and atmospheric conditions and viewing geometries. This study analyzes calibration strategies while considering some of the most critical factors that need to be taken into account when building a calibration dataset, covering the full dynamic range of relevant variables. A sensitivity analysis of split-windows and single channel algorithms revealed that selecting a set of atmospheric profiles that spans the full range of surface temperatures and total column water vapor combinations that are physically possible seems beneficial for the quality of the regression model. However, the calibration is extremely sensitive to the low-level structure of the atmosphere, indicating that the presence of atmospheric boundary layer features such as temperature inversions or strong vertical gradients of thermodynamic properties may affect LST retrievals in a non-trivial way. This article describes the criteria established in the EUMETSAT Land Surface Analysis—Satellite Application Facility to calibrate its LST algorithms, applied both for current and forthcoming sensors.http://www.mdpi.com/2072-4292/8/10/808land surface temperaturethermal infraredcalibrationgeneralized split-windowmono-windowdatabaseradiative transfer |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
João P. A. Martins Isabel F. Trigo Virgílio A. Bento Carlos da Camara |
spellingShingle |
João P. A. Martins Isabel F. Trigo Virgílio A. Bento Carlos da Camara A Physically Constrained Calibration Database for Land Surface Temperature Using Infrared Retrieval Algorithms Remote Sensing land surface temperature thermal infrared calibration generalized split-window mono-window database radiative transfer |
author_facet |
João P. A. Martins Isabel F. Trigo Virgílio A. Bento Carlos da Camara |
author_sort |
João P. A. Martins |
title |
A Physically Constrained Calibration Database for Land Surface Temperature Using Infrared Retrieval Algorithms |
title_short |
A Physically Constrained Calibration Database for Land Surface Temperature Using Infrared Retrieval Algorithms |
title_full |
A Physically Constrained Calibration Database for Land Surface Temperature Using Infrared Retrieval Algorithms |
title_fullStr |
A Physically Constrained Calibration Database for Land Surface Temperature Using Infrared Retrieval Algorithms |
title_full_unstemmed |
A Physically Constrained Calibration Database for Land Surface Temperature Using Infrared Retrieval Algorithms |
title_sort |
physically constrained calibration database for land surface temperature using infrared retrieval algorithms |
publisher |
MDPI AG |
series |
Remote Sensing |
issn |
2072-4292 |
publishDate |
2016-09-01 |
description |
Land surface temperature (LST) is routinely retrieved from remote sensing instruments using semi-empirical relationships between top of atmosphere (TOA) radiances and LST, using ancillary data such as total column water vapor or emissivity. These algorithms are calibrated using a set of forward radiative transfer simulations that return the TOA radiances given the LST and the thermodynamic profiles. The simulations are done in order to cover a wide range of surface and atmospheric conditions and viewing geometries. This study analyzes calibration strategies while considering some of the most critical factors that need to be taken into account when building a calibration dataset, covering the full dynamic range of relevant variables. A sensitivity analysis of split-windows and single channel algorithms revealed that selecting a set of atmospheric profiles that spans the full range of surface temperatures and total column water vapor combinations that are physically possible seems beneficial for the quality of the regression model. However, the calibration is extremely sensitive to the low-level structure of the atmosphere, indicating that the presence of atmospheric boundary layer features such as temperature inversions or strong vertical gradients of thermodynamic properties may affect LST retrievals in a non-trivial way. This article describes the criteria established in the EUMETSAT Land Surface Analysis—Satellite Application Facility to calibrate its LST algorithms, applied both for current and forthcoming sensors. |
topic |
land surface temperature thermal infrared calibration generalized split-window mono-window database radiative transfer |
url |
http://www.mdpi.com/2072-4292/8/10/808 |
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