1.
Appl Opt
; 7(6): 1137-40, 1968 Jun 01.
Artigo
em Inglês
| MEDLINE
| ID: mdl-20068752
RESUMO
Spectra in the 8.5-16-micro interval, taken at various altitudes over relatively uniform desert terrain, show attenuation of upwelling radiation by atmospheric gases and haze through the entire spectral interval. Equivalent blackbody temperatures, even in the clearest part of the window, show a drop that could introduce serious errors into remote sensing of surface temperatures. Surface emissivity characteristies are discernible at low altitudes but are somewhat masked by ozone at 10-km altitudes.