1998
DOI: 10.1006/icar.1997.5887
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The Microwave Absorption and Abundance of Sulfuric Acid Vapor in the Venus Atmosphere Based on New Laboratory Measurements

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Cited by 77 publications
(74 citation statements)
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References 20 publications
(11 reference statements)
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“…Unfortunately, at the altitude of the cloud base of Venus, the measurement errors in radio occultation profile analysis are beginning to become quite large. Previous studies by Kolodner and Steffes (1998) indicate large vertical and meridional variations, and even significant inversions in the sulfuric acid vapor mixing ratio below cloud base. Such strong observed variations must be indicative either of a tremendous amount of vertical overturning in the subcloud region, or of significant measurement uncertainties.…”
Section: Reduced Acid Vapor Boundary Conditionmentioning
confidence: 84%
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“…Unfortunately, at the altitude of the cloud base of Venus, the measurement errors in radio occultation profile analysis are beginning to become quite large. Previous studies by Kolodner and Steffes (1998) indicate large vertical and meridional variations, and even significant inversions in the sulfuric acid vapor mixing ratio below cloud base. Such strong observed variations must be indicative either of a tremendous amount of vertical overturning in the subcloud region, or of significant measurement uncertainties.…”
Section: Reduced Acid Vapor Boundary Conditionmentioning
confidence: 84%
“…In all simulations presented here, I define a water vapor boundary condition of 30 ppmv at 40 km altitude (Pollack et al 1993). Similarly, a sulfuric acid boundary condition of 10 ppmv is set at 40 km altitude Kolodner and Steffes (1998), except in a subset of simulations in which this boundary condition is reduced to 5 ppmv. The top boundary condition for vapors assumes a constant mixing ratio above the top boundary.…”
Section: Vapor Boundary and Initial Conditionsmentioning
confidence: 99%
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“…[12] Turning from infrared to radio frequencies, radio occultation can be used to measure vertical profiles of gaseous H 2 SO 4 at altitudes down to $35 km; a recent reanalysis of six individual occultations from the Magellan and Mariner 10 orbiters found H 2 SO 4 abundances at 41 km s ranging from 0 ppm to 8 ppm [Kolodner and Steffes, 1998], and it certainly seems reasonable to suggest that a larger range of variation might be found if more occultations were analysed. The decomposition of each H 2 SO 4 molecule would yield a molecule of H 2 O, so this range of >8 ppm of H 2 SO 4 at 41 km would be expected to yield a variation of >8 ppm in water vapour abundance at this altitude, and thus is entirely consistent with the present results from VIRTIS.…”
Section: Discussionmentioning
confidence: 99%
“…This expression is slightly modified from that given in Kolodner and Steffes (1998) as per M. A. Kolodner (personal communication).…”
Section: Radiative Transfer Modelingmentioning
confidence: 98%