The Long-Term Effects of Surface Frosts, Seasonal Atmospheric Water Variation and Ice Fraction-Dependent Thermal Conductivity on Martian Ground Ice

Details The Long-Term Effects of Surface Frosts, Seasonal Atmospheric Water Variation and Ice Fraction-Dependent Thermal Conductivity on Martian Ground Ice The Long-Term Effects of Surface Frosts, Seasonal Atmospheric Water Variation and Ice Fraction-Dependent Thermal Conductivity on Martian Ground Ice

Mar 2012

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2012lpi....43.2808b&link_type=abstract

43rd Lunar and Planetary Science Conference, held March 19–23, 2012 at The Woodlands, Texas. LPI Contribution No. 1659, id.2808

Physics

Scientific paper

We use a 1-D time-dependent model to simulate martian ground ice
evolution over the past ~1 Myr. Our goal is to quantify and understand
the effects of some known processes (see title) on ground ice
growth/retreat rates.

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