Air temperature estimation with MSG-SEVIRI data: Calibration and validation of the TVX algorithm for the Iberian Peninsula |
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Authors: | Héctor Nieto Inge Sandholt |
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Affiliation: | a Department of Geography, University of Alcalá, Colegios 2, 28801, Alcalá de Henares, Spainb Department of Geography and Geology, University of Copenhagen, Øster Volgade 10, 1350, Copenhagen K, Denmarkc GEUS, Geological Survey of Denmark and Greenland, Øster Volgade 10, 1350, Copenhagen K, Denmark |
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Abstract: | Air temperature can be estimated from remote sensing by combining information in thermal infrared and optical wavelengths. The empirical TVX algorithm is based on an estimated linear relationship between observed Land Surface Temperature (LST) and a Spectral Vegetation Index (NDVI). Air temperature is assumed to be equal to the LST corresponding to the effective full vegetation cover, and is found by extrapolating the line to a maximum value of NDVImax. The algorithm has been tested and reported in the literature previously. However, the effect of vegetation types and climates and the potential variation in NDVI of the effective full cover has not been subject for investigation. The present study proposes a novel methodology to estimate NDVImax that uses observed air temperature to calibrate the NDVImax for each vegetation type. To assess the validity of this methodology, we have compared the accuracy of estimates using the new NDVImax and the previous NDVImax that have been proposed in literature with MSG-SEVIRI images in Spain during the year 2005. In addition, a spatio-temporal assessment of residuals has been performed to evaluate the accuracy of retrievals in terms of daily and seasonal variation, land cover, landscape heterogeneity and topography. Results showed that the new calibrated NDVImax perform well, with a Mean Absolute Error ranging between 2.8 °C and 4 °C. In addition, vegetation-specific NDVImax improve the accuracy compared with a unique NDVImax. |
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Keywords: | MSG-SEVIRI Air temperature TVX algorithm Land Surface Temperature NDVI |
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