Logo image
Use of the 4.5- to 5- m atmospheric window for background temperature evaluation
Conference proceeding

Use of the 4.5- to 5- m atmospheric window for background temperature evaluation

Eli T Talmor, Leslie S Balfour, Avshalom Pasternak and Baruch Ben-Dor
Proceedings of SPIE, v 1971(1), pp 127-135
13 Aug 1993

Abstract

Spectral radiance of various background elements (e.g., vegetation, rocks, snow and concrete) were measured in the 4.5 - 5 micrometers atmospheric window, both during the day and night. Effective temperatures of these surfaces were calculated and an attempt was made to evaluate true temperatures as well. The results are quite satisfactory, probably due to the following reasons: (1) The emissivity of most natural surfaces in this spectral region is high. Therefore the non-thermal (reflected solar component of the radiance) is small. (2) The spectral variation of the emissivity of most natural surfaces in this spectral region is very small, thus facilitating the evaluation of contact surface temperature. The results suggest the feasibility of using the 4.5 - 5 micrometers atmospheric window for background temperature evaluation.

Metrics

11 Record Views

Details

InCites Highlights

Data related to this publication, from InCites Benchmarking & Analytics tool:

Web of Science research areas
Engineering, Aerospace
Meteorology & Atmospheric Sciences
Optics
Logo image