Spectral imaging of martian water ice clouds and their diurnal behavior during the 1999 aphelion season (Ls = 130°)

Details Spectral imaging of martian water ice clouds and their diurnal behavior during the 1999 aphelion season (Ls = 130°) Spectral imaging of martian water ice clouds and their diurnal behavior during the 1999 aphelion season (Ls = 130°)

Feb 2003

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003icar..161..297g&link_type=abstract

Icarus, Volume 161, Issue 2, p. 297-318.

Computer Science

12

Scientific paper

We report high-spectral-resolution (λ/δλ = 800-2300) near-infrared mapping observations of Mars at Ls = 130° (April 1999), which were obtained by drift-scanning the cryogenic long-slit spectrometer at the KPNO 2.2-m telescope across the disk. Data were reformatted into calibrated spectral image cubes (x,y,λ) spanning 2.19 to 4.12 μm, which distinguish atmospheric CO2 features, solar lines, and surface and aerosol features. Maps of relative band depth between 3.0 and 3.5 μm trace water ice clouds and show the diurnal evolution of features in the persistent northern summer aphelion cloud belt, which was mapped contemporaneously but at fixed local time by the Mars Global Surveyor Thermal Emission Spectrometer (MGS/TES). Cloud optical depth, particle sizes, and ice aerosol content were estimated using a two-stream, single-layer scattering model, with Mie coefficients derived from recently published ice optical constants, followed by a linear spectral deconvolution process. A comparison of data and model spectra shows evaporating nighttime clouds in the morning followed by afternoon growth of a prominent orographic cloud feature on the west flank of Elysium Mons. Cloud optical depth at 3.2 μm evolved to 0.28 +/- 0.13 and ice aerosol column abundance to 0.9 +/- 0.3 pr μm in the afternoon. Column abundances as large as 0.17 pr μm were retrieved in nonorographic clouds within the aphelion cloud band around midday. These clouds exhibit a modest decline in optical depth during the afternoon. Results show that ice particle radii from <2 μm to >4 μm exist in both cloud types. However, large particles dominate the spectra, consistent with recent MGS/TES emission phase function measurements of aphelion cloud aerosol properties.

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