1998
DOI: 10.1029/98gl00236
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CIRRIS‐1A limb spectral measurements of mesospheric 9.6‐µm airglow and ozone

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Cited by 16 publications
(12 citation statements)
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References 17 publications
(6 reference statements)
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“…Rawlins et al [1985] derived a statistical vibrational distribution which decreases with excitation. This approach was used by Mlynczak and Drayson [1990a] (Simple Single Model), Fichet et al [1992], and Zhou et al [1998]; (2) An ''inverse Rawlins distribution'' (F. J. Martín-Torres et al, manuscript in preparation, 2002), which assumes that the whole manifold of vibrational states below the energy dissociation limit are populated after recombination and favors the population of the higher vibrational states.…”
Section: Non-lte Processesmentioning
confidence: 99%
See 1 more Smart Citation
“…Rawlins et al [1985] derived a statistical vibrational distribution which decreases with excitation. This approach was used by Mlynczak and Drayson [1990a] (Simple Single Model), Fichet et al [1992], and Zhou et al [1998]; (2) An ''inverse Rawlins distribution'' (F. J. Martín-Torres et al, manuscript in preparation, 2002), which assumes that the whole manifold of vibrational states below the energy dissociation limit are populated after recombination and favors the population of the higher vibrational states.…”
Section: Non-lte Processesmentioning
confidence: 99%
“…Several rocket borne measurements of mesospheric ozone infrared emissions have been performed [e.g., Rawlins et al, 1985;Green et al, 1986;Grossmann and Vollmann, 1997]. Global upper mesospheric ozone infrared emission measurements have been analyzed by Zhou et al [1998] and Mill et al [1994].…”
Section: Introductionmentioning
confidence: 99%
“…Figure 1 presents examples of the height distribution of the O 3 concentration in the mesosphere during daytime, obtained from measurements and as a result of theoretical studies. Measurements show substantial diurnal variations at mesospheric altitudes with maximum concentrations at nighttime and a secondary peak above 80 km (Llewellyn and Witt, 1977;Weeks et al, 1972Weeks et al, , 1978Wilson and Schwartz, 1981;Ulwick et al, 1987;Zommerfields et al, 1989;Zhou et al, 1998;Sandor et al, 1997;Gumbel et al, 1998;Fussen et al, 2000;Kaufmann et al, 2003;Polyakov et al, 2005;Kyrölä et al, 2006).…”
Section: Height Profiles Of Ozone In the Mesospherementioning
confidence: 99%
“…Calibrating FIRST required addressing basic issues of absolute radiometric response, frequency scale, instrument line shape, phase alignment and self-apodization. Techniques for quantifying and modeling these effects were applied to FIRST 10,11,12,13,14,15 during its calibration. For Earth scene calibration, FIRST utilized the same calibration scheme adopted by the NPOESS Cross Track Infrared Sounder (CrIS) sensor with calibration information from space view (cold BB) and then the warm flight blackbody.…”
Section: First Calibrationmentioning
confidence: 99%