LAUSR

Even if water vapor is a minor species in the Martian atmosphere it plays an important role in the planet"s climate. Major efforts were made to understand water vapor distribution during the last decades. Its seasonal cycle was studied in detail using nadir measurements by TES/Mars Global Surveyor, three experiments onboard Mars-Express, SPICAM, OMEGA and PFS, and by CRISM/Mars Reconnaissance Orbiter. In contrast to column abundance, the climatology of water vapor vertical distribution was scarcely documented until recently. The vertical distribution gauges multiple processes controlling the Martian water cycle, including the cloud formation with condensation, evaporation and sedimentation, sublimation and condensation on polar caps, the photodissociation and escape processes, and surface-atmosphere exchange [1]. A few spectrometers, SPICAM on MEX and ACS and NOMAD on TGO, carry out now the measurements of water vertical distribution from Mars" orbit. They have got already prominent results as a supersatutation of water during the aphelion and perihelion season [2,3], high altitude water during global dust storms of MY28 [4] and MY34 [3,5] and high perihelion water in MY34 [3,6].ObservationsIn this work, we present the first multi-annual survey of water vapor in the middle atmosphere of Mars based on SPICAM/MEx occultation measurements. SPICAM IR is an infrared spectrometer employing an Acousto-Optic Tunable Filter (AOTF) working in the spectral range of 1-1.7 μm with a spectral resolution of 3.5-4 cm-1, nearly constant in wavenumbers [7]. SPICAM can observe the H2O vertical distribution using the 1.38 µm band, the CO2 density in the 1.43 µm band, and the aerosol density and size distribution using several continuum portions of the spectrum. We analyzed Eight Martian years of H2O vertical distribution from MY27 to MY34.Figure 1. Seasonal-latitudinal coverage of SPICAM observations in solar occultations for eight Martian years. The open circles mark faulty observations inapplicable for retrieval.ResultsThe upper limit of water density detected by SPICAM varies from 50-60 km in aphelion to 70-90 km in perihelion. In aphelion (Ls=0-120°), the H2O mixing ratio 100 ppm at 40-90 km was observed at Ls=240-290° in high and middle southern latitudes. We also present a comparison of two global dust storms of MY28 and 34 and we concluded that the GDS of MY28, coincident with southern summer solstice, shows a noticeably higher water increase.