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Sublimation of terrestrial permafrost and the implications for ice-loss processes on Mars
Sublimation of ice is rate-controlled by vapor transport away from its outer surface and may have generated landforms on Mars. In ice-cemented ground (permafrost), the lag of soil particles remaining after ice loss decreases subsequent sublimation. Varying soil-ice ratios lead to differential lag de...
| Autores principales: | , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Nature Publishing Group UK
2019
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6461685/ https://www.ncbi.nlm.nih.gov/pubmed/30979886 http://dx.doi.org/10.1038/s41467-019-09410-8 |