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Thermal Detectability of Subsurface Water Ice on Mars: A Comparative Analysis for the Subsurface Water Ice Mapping (SWIM) Project

  • Authors: Hanna G. Sizemore, Asmin V. Pathare, Colin M. Dundas, Nathaniel E. Putzig, Gareth A. Morgan, Matthew R. Perry, Michael T. Mellon, Zachary M. Bain, Samuel W. Courville

Hanna G. Sizemore et al 2026 The Planetary Science Journal 7 .

  • Provider: AAS Journals

Caption: Figure 12.

Seasonal temperature curves at 45°N latitude as predicted by (a) S. Piqueux et al. (2019) using KRC and (b) SWIM23 using MARSTHERM. The gray zone corresponds to the period of time in the Martian orbit (Ls*) when surface temperature is insensitive to the distribution of buried ice. Note that MARSTHERM predicts less temperature separation with respect to ice table depth and a wider range of Ls* with varying surface TI than KRC.

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