Sublimation of terrestrial permafrost and the implications for ice-loss processes on Mars
Sublimation of ice is believed to have generated a variety of landforms on Mars and other planetary bodies. Here the authors show the first long-term in situ effective diffusion coefficient of terrestrial ice-free loess (Mars analog soil), scaled to Mars average pressure, temperature and CO2 atmosph...
Guardado en:
Autores principales: | , |
---|---|
Formato: | article |
Lenguaje: | EN |
Publicado: |
Nature Portfolio
2019
|
Materias: | |
Acceso en línea: | https://doaj.org/article/9f30e5d8e32e4880ba15e1be01794d95 |
Etiquetas: |
Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
|
id |
oai:doaj.org-article:9f30e5d8e32e4880ba15e1be01794d95 |
---|---|
record_format |
dspace |
spelling |
oai:doaj.org-article:9f30e5d8e32e4880ba15e1be01794d952021-12-02T15:36:22ZSublimation of terrestrial permafrost and the implications for ice-loss processes on Mars10.1038/s41467-019-09410-82041-1723https://doaj.org/article/9f30e5d8e32e4880ba15e1be01794d952019-04-01T00:00:00Zhttps://doi.org/10.1038/s41467-019-09410-8https://doaj.org/toc/2041-1723Sublimation of ice is believed to have generated a variety of landforms on Mars and other planetary bodies. Here the authors show the first long-term in situ effective diffusion coefficient of terrestrial ice-free loess (Mars analog soil), scaled to Mars average pressure, temperature and CO2 atmosphere.Thomas A. DouglasMichael T. MellonNature PortfolioarticleScienceQENNature Communications, Vol 10, Iss 1, Pp 1-9 (2019) |
institution |
DOAJ |
collection |
DOAJ |
language |
EN |
topic |
Science Q |
spellingShingle |
Science Q Thomas A. Douglas Michael T. Mellon Sublimation of terrestrial permafrost and the implications for ice-loss processes on Mars |
description |
Sublimation of ice is believed to have generated a variety of landforms on Mars and other planetary bodies. Here the authors show the first long-term in situ effective diffusion coefficient of terrestrial ice-free loess (Mars analog soil), scaled to Mars average pressure, temperature and CO2 atmosphere. |
format |
article |
author |
Thomas A. Douglas Michael T. Mellon |
author_facet |
Thomas A. Douglas Michael T. Mellon |
author_sort |
Thomas A. Douglas |
title |
Sublimation of terrestrial permafrost and the implications for ice-loss processes on Mars |
title_short |
Sublimation of terrestrial permafrost and the implications for ice-loss processes on Mars |
title_full |
Sublimation of terrestrial permafrost and the implications for ice-loss processes on Mars |
title_fullStr |
Sublimation of terrestrial permafrost and the implications for ice-loss processes on Mars |
title_full_unstemmed |
Sublimation of terrestrial permafrost and the implications for ice-loss processes on Mars |
title_sort |
sublimation of terrestrial permafrost and the implications for ice-loss processes on mars |
publisher |
Nature Portfolio |
publishDate |
2019 |
url |
https://doaj.org/article/9f30e5d8e32e4880ba15e1be01794d95 |
work_keys_str_mv |
AT thomasadouglas sublimationofterrestrialpermafrostandtheimplicationsforicelossprocessesonmars AT michaeltmellon sublimationofterrestrialpermafrostandtheimplicationsforicelossprocessesonmars |
_version_ |
1718386306190409728 |