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Surface temperature of Martian regolith with polygonal features: influence of the subsurface water ice

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Kossacki,  Konrad J.
Department Planets and Comets, Max Planck Institute for Solar System Research, Max Planck Society;

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Markiewicz,  Wojciech J.
Department Planets and Comets, Max Planck Institute for Solar System Research, Max Planck Society;
MPI for Aeronomy, Max Planck Institute for Solar System Research, Max Planck Society;

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Kossacki, K. J., Markiewicz, W. J., & Smith, M. D. (2003). Surface temperature of Martian regolith with polygonal features: influence of the subsurface water ice. Planetary and Space Science, 51, 569-580.


Cite as: http://hdl.handle.net/11858/00-001M-0000-0014-EF31-7
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