Orbital Variations of the Rheology and Sublimation of the Martian Polar Layered Deposits: Glaciological Implications

Details Orbital Variations of the Rheology and Sublimation of the Martian Polar Layered Deposits: Glaciological Implications Orbital Variations of the Rheology and Sublimation of the Martian Polar Layered Deposits: Glaciological Implications

Aug 2000

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2000mpse.conf..145p&link_type=abstract

International Conference on Mars Polar Science and Exploration, p. 145

Mathematics

Logic

Mars (Planet), Rheology, Sublimation, Polar Regions, Geochronology, Glaciology, Ablation, Flow Velocity, Insolation

Scientific paper

Martian obliquity deviates aperiodically from its current Earth-like value of 25 deg, often surpassing 45 deg within the last 20 Myr. We calculate the effects of the corresponding variations in insolation upon first the rheology and then the sublimation of the Polar Layered Deposits (PLD). We then consider the glaciological implications of this simultaneous increase in flow and ablation rates. Additional information is contained in the original extended abstract.

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