Vertical distribution of ozone on Mars as measured by SPICAM/Mars Express using stellar occultations

Details Vertical distribution of ozone on Mars as measured by SPICAM/Mars Express using stellar occultations Vertical distribution of ozone on Mars as measured by SPICAM/Mars Express using stellar occultations

Sep 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006jgre..11109s05l&link_type=abstract

Journal of Geophysical Research, Volume 111, Issue E9, CiteID E09S05

Physics

9

Planetary Sciences: Solar System Objects: Mars, Planetary Sciences: Solid Surface Planets: Composition (1060, 3672), Planetary Sciences: Solid Surface Planets: Remote Sensing, Atmospheric Composition And Structure: Planetary Atmospheres (5210, 5405, 5704)

Scientific paper

The ultraviolet spectrometer of the SPICAM instrument on board the European Mars Express mission has performed stellar occultations to probe the atmosphere. Vertical profiles of ozone are retrieved from inversion of transmission spectra in the altitude range 20-30 to 70 km. They are analyzed here as functions of latitude and season of the observations. These occultations have been monitored on the night side, from northern spring equinox (Ls = 8°) to northern winter solstice (Ls = 270°). The profiles show the presence of two ozone layers: (1) one located near the surface, the top of which is visible below 30 km altitude, and (2) one layer located in the altitude range 30 to 60 km, a feature that is highly variable with latitude and season. This layer is first seen after Ls = 11°, and the ozone abundance at the peak tends to increase until Ls ~ 40°, when it stabilizes around 6-8 × 109 cm-3. After southern winter solstice (Ls ~ 100°), the peak abundance starts decreasing again, and this ozone layer is no longer detected after Ls ~ 130°. A recent model (Lefèvre et al., 2004) predicted the presence of these ozone layers, the altitude one being only present at night. Though the agreement between model and observations is quite good, this nocturnal altitude layer is present in SPICAM data over a less extended period than predicted. Though a possible role of heterogeneous chemistry is not excluded, this difference is probably linked to the seasonal evolution of the vertical distribution of water vapor.

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