A
Technique to Estimate the Emissivity of a Volcanic
Area at Wavelengths of Avhrr Tir
Channels
In this work a study about
the emissivity and atmospheric effects related to the
Land Surface Temperature determination is shown. For this purpose, a particular
test area situated over 2300 m altitude in a volcanic terrain at Las Caņadas National Park (Canary Islands) has been selected. In this zone,
the prevailing trade winds system make the highest
water vapor content to be concentrated under this
altitude. In order to analyze the effect of this absorbent gas on the
atmospheric correction, a preliminary study using radiosounding
profiles and radiances simulated with MODTRAN radiance/transmittance code is
made. The results of this analysis suggest that if its contribution is
negligible or can be easily parameterized, the effective emissivity
could be calculated by tuning its value in the radiative
transfer equation and using a sufficiently representative number of in situ
measurements together with the corresponding coincident satellite measurements.