1966
DOI: 10.1175/1520-0493(1966)094<0367:imoatp>2.3.co;2
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Indirect Measurements of Atmospheric Temperature Profiles From Satellites: Iii. The Spectrometers and Experiments

Abstract: Three spectrometers and associated experiments are described. The work reviewed comprises the early experimental phases of a program to develop a satellite infrared spectrometer capable of making radiometric measurements in the 15-micron carbon dioxide band needed for deduction of atmospheric temperature profiles. Initially, a simplified, breadboard spectrometer with four spectral channels was used to determine the temperature profile of the lower atmosphere from the ground. Next, a commercial spectrophotomete… Show more

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Cited by 13 publications
(6 citation statements)
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“…The usefulness of measuring atmospheric T and WV in order to diagnose the state of the atmosphere lead to the development of satellite‐based sounding instruments over 40 years ago [ Hilleary et al , 1966; James , 1967; Yates , 1970; Chesters et al , 1986], beginning with the U.S. Satellite Infrared Spectrometer (SIRS) and Infrared Interferometer Spectrometer (IRIS) onboard Nimbus 3, launched in 1969 [ Wark and Hilleary , 1969; Hayden , 1971; Wick , 1971; Smith , 1972]. SIRS and IRIS were capable of remotely sensing atmospheric T structures by using statistical relationships and regression methods [ Kaplan et al , 1977; Westwater and Strand , 1968; Smith et al , 1970; Crosby et al , 1973; Fritz , 1977].…”
Section: Introductionmentioning
confidence: 99%
“…The usefulness of measuring atmospheric T and WV in order to diagnose the state of the atmosphere lead to the development of satellite‐based sounding instruments over 40 years ago [ Hilleary et al , 1966; James , 1967; Yates , 1970; Chesters et al , 1986], beginning with the U.S. Satellite Infrared Spectrometer (SIRS) and Infrared Interferometer Spectrometer (IRIS) onboard Nimbus 3, launched in 1969 [ Wark and Hilleary , 1969; Hayden , 1971; Wick , 1971; Smith , 1972]. SIRS and IRIS were capable of remotely sensing atmospheric T structures by using statistical relationships and regression methods [ Kaplan et al , 1977; Westwater and Strand , 1968; Smith et al , 1970; Crosby et al , 1973; Fritz , 1977].…”
Section: Introductionmentioning
confidence: 99%
“…It has been pointed out [IO] that when experimental data with relatively small errors are used in equation (l), the errors in the resulting solution can be enormously large. This observation was clearly demonstrated [5] when the "breadboard" model of the satellite infrared spectrometer was used to sound the atmosphere from the ground t o provide experimental data for preliminary analyses. During those experiments, however, the satellite spectrometer incorporated only four frequency channels.…”
Section: Introductionmentioning
confidence: 89%
“…The spectrometer response was calibrated as a function of spectral radiance with two blackbodies [5]. The block diagram for calibration and observation is shown in figure 1.…”
Section: Measurement Of Downward Spectral Radiancementioning
confidence: 99%
“…A variety of instrumental techniques will be used including conventional, fixed grating, multidetector spectrometers, Michelson interferometers, and spectrometers in which spectral separation is achieved by rotating wedges of continuous interference layers. (Hilleary et al 1966, Hanel and Chaney 1966,5 Hovis 1966. Improvements i n spatial and spectral resolution by about one to two orders of magnitude can be expected when highly cooled infrared detectors (77'K) can be accommodated routinely on spacecraft.…”
Section: Sensing O F Radiation From the Lower Atmosphere A Physical mentioning
confidence: 99%
“…Complete temperature profiles have not yet been measured from satellites, but plans for such measurements exist and encouraging results have been obtained from attempts at inverting radiometric data taken with balloon borne instruments (Hilleary et al, 1966).…”
Section: Atmospheric Temperature and Moisturementioning
confidence: 99%