METHANE AND WATER ON MARS: MAPS OF ACTIVE REGIONS AND THEIR SEASONAL VARIABILITY

Details METHANE AND WATER ON MARS: MAPS OF ACTIVE REGIONS AND THEIR SEASONAL VARIABILITY METHANE AND WATER ON MARS: MAPS OF ACTIVE REGIONS AND THEIR SEASONAL VARIABILITY

Dec 2009

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2009agufm.p41b..01v&link_type=abstract

American Geophysical Union, Fall Meeting 2009, abstract #P41B-01

Biology

[0343] Atmospheric Composition And Structure / Planetary Atmospheres, [5200] Planetary Sciences: Astrobiology, [6225] Planetary Sciences: Solar System Objects / Mars

Scientific paper

We have detected methane on Mars, and measured it simultaneously with water using powerful ground-based telescopes [1, 2]. Its presence in such a strongly oxidized atmosphere (CO2: 95.3%) requires recent release; the ultimate origin of this methane is uncertain, but it could either be abiotic or biotic. On Earth, methane is produced primarily by biology, with a small fraction produced by abiotic means. The sources and sinks of hydrogen-bearing species (e.g., H2O and CH4) on Mars are still poorly known. In particular, the roles of the regolith and the sub-surface hydrogen reservoirs in the Martian water cycle have been broadly studied, but have not been conclusively quantified. If water is being released from the sub-surface or shares a common source with other H-bearing species, we might see correlations among them. Previous searches for such correlations have been precluded because of the lack of simultaneity of the measurements and the intrinsic variability of water on Mars, which is a condensable whose total local abundance is partitioned among several competing phases controlled largely by temperature (ensuring its variability on a variety of time scales, from diurnal to seasonal to epochal). We sampled multiple spectral lines of methane and water vapor on Mars in a campaign spanning seven years (three Mars years; 1999-2006) and sampling three seasons on Mars. Data were ac-quired using long-slit infrared spectrometers: CSHELL (Cryogenic Echelle Spectrograph) at NASA-IRTF (Infrared Telescope Facility) and NIRSPEC (Near Infrared Spectrograph) at Keck 2. These instruments offer spatially-resolved spectra with the high spectral resolving power (λ/δλ ~ 40,000) needed to reduce confusion among telluric, Martian, and Fraunhofer lines (in reflected solar radiation). Since 2005, we greatly improved our data processing algorithms and increased the sensitivity of our measurements by an order of magnitude. Using these new techniques, we detected multiple lines of methane on Mars [1] and discovered two new band sys-tems of isotopic CO2 (at 3.3 and 3.7 μm) that can interfere with signatures of CH4 and HDO [3, 4]. The spectral signatures of these isotopic CO2 transitions may affect searches based on low spectral resolution methods, but they do not affect the searches reported herein. We present the spatial distributions of methane and water-vapor on Mars extracted from our seven-year spectral database, and we compare these with geological parameters. Both gases are depleted at vernal equinox but are enhanced in warm seasons (spring/summer), though often with dissimilar spatial distributions. In Northern Summer we observe a polar outburst of water but no methane, while in Southern Spring we observe release of abundant methane but little water. Regions of methane release appear mainly over ancient terrain (Noachian/Hesperian, older than 3 billion years) known to have a rich hydration history. [1] Mumma et al. (2009) Science 323:1041-1045. [2] Villanueva et al. (2009), submitted. [3] Villanueva et al. (2008) Icarus 195(1):34-44. [4] Villanueva et al. (2008) JQSRT 109(6):883-894.

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