Abstract
Abstract An integral relation has been obtained between variations of the brightness temperature for ground-based microwave radiometry and meteorological parameters of the atmosphere which permits a general approach to the statement of inverse problems of thermal and humidity sensing in the microwave range Statistical estimations of accuracy for recovering low-altitude temperature and humidity profiles are given. Using the example of ammonia pollution of the atmosphere (over its radiation in the region of the inverse resonance λ ∼ 1.25cm) possibilities are illustrated of remote-sensing methods for the definition of constituents of an industrial origin Problems are considered for the use of remote-sensing data in real-time monitoring of the astronomical refraction and the electrical path length of the atmosphere in the radio range.
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