Sovremennye problemy distantsionnogo zondirovaniya Zemli iz kosmosa, 2009. Issue.6. Vol.1. P. 216-219
Estimation albedo surfaces of the Earth in an infra-red range for
transition from radiating temperatures to thermodynamic
Всероссийский научно-исследовательский институт рыбного хозяйства и океанографии, 107140 Москва, Верхняя Красносельская, 17
At remote sounding the Earth in an infra-red range of a spectrum turn out radiating, instead
of thermodynamic temperatures of terrestrial covers, distinctions of temperatures at times exceed
5 K. It is differences of factor of radiating of objects from 1. Spectral measurements of radiation
leaving from the Earth are necessary for an estimation of current values of factor of radiation, for
example, data of radiometers AVHRR or MODIS. The major at corresponding calculations is
correction on deforming influence of an atmosphere, thus sizes albedo radiation reflected from an
aerosol have special value. For an estimation of current sizes albedo radiation reflected from an
aerosol, it is necessary to consider features of the wave and corpuscular nature of radiation.
Keywords: radiating and thermodynamic temperatures, radiating, correction on deforming influence of an atmosphere, aerosol
Full text