Thermal infrared data of the Digital Airborne Imaging Spectrometer ( DAIS),
whose channels 74-79 are in the 8-13 mum waveband region, were analysed wi
th the aim of recovering land surface temperature ( LST). DAIS images were
acquired over an experimental site where field and laboratory emissivity me
asurements were performed, and these were used to recover the LST from the
six DAIS thermal channels. Atmospheric correction of DAIS data was calculat
ed by means of a nearby radiosounding and a radiative transfer model. DAIS
derived LSTs were compared with ground measurements of LST made coincidenta
lly for a few test fields, the central DAIS channels yielding temperatures
up to 10 degreesC higher than ground measurements. A linear calibration was
performed using in situ measurements of temperature and emissivity for two
reference fields, and the large differences in temperature were then consi
derably reduced. Temperatures obtained from DAIS channel 79 agreed with the
in situ measurements within +/-2 degreesC. This channel seemed the most re
liable for deriving accurate LSTs in the dataset analysed here.