1970
DOI: 10.1016/s0034-4257(70)80001-3
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Effects of atmospheric path on airbornemultispectral sensors

Abstract: Experimental data were acquired for a study of the effects of variable atmospheric path on the spectral signals obtained by remote sensors in the optical region of the spectrum. Multichannel optical-mechanical scanners which provide calibrated apparent spectral radiance data were flown over agricultural test sites, and passes were made at several different altitudes between 2000 and 10,000 ft. The quantitative results compare favorably with qualitative theoretical predictions. Optical-mechanical scanners and a… Show more

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Cited by 15 publications
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“…It varies with the weather, the time of day, the altitude, and with the nature of the suspended particles, but it is accepted that haze is present in the atmosphere to some extent all over the world. " Horvath, Braithwaite and Polcyn (1969) in a useful discussion of the effect of sensor altitude on the apparent radiance of an object (which fills the sensor's instantaneous field of view) note that the actual radiance is modulated by both (1) atmospheric attenuation through absorption or scattering of the radiation reflected or emitted from the object, and 2atmospheric scattering and emission of unwanted radiation into the field of view. The latter effect is the most significant in the 400-900 n.m. region in increasing the total scene radiance and reducing target radiance contrast.…”
mentioning
confidence: 99%
“…It varies with the weather, the time of day, the altitude, and with the nature of the suspended particles, but it is accepted that haze is present in the atmosphere to some extent all over the world. " Horvath, Braithwaite and Polcyn (1969) in a useful discussion of the effect of sensor altitude on the apparent radiance of an object (which fills the sensor's instantaneous field of view) note that the actual radiance is modulated by both (1) atmospheric attenuation through absorption or scattering of the radiation reflected or emitted from the object, and 2atmospheric scattering and emission of unwanted radiation into the field of view. The latter effect is the most significant in the 400-900 n.m. region in increasing the total scene radiance and reducing target radiance contrast.…”
mentioning
confidence: 99%