Islands of ice on Mars and Pluto
Ice sheets, such as the polar layered deposits (PLDs) of Mars, are of great interest as records of past climate. Smaller outlier ice deposits near the north and south PLDs are likely more sensitive to climate changes and thus may hold information about more recent climate history. However, the south...
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ftunivbern:oai:boris.unibe.ch:143793 2023-08-20T04:07:16+02:00 Islands of ice on Mars and Pluto Sori, Michael M. Bapst, Jonathan Becerra, Patricio Byrne, Shane 2019 application/pdf https://boris.unibe.ch/143793/1/2018JE005861.pdf https://boris.unibe.ch/143793/ eng eng Wiley https://boris.unibe.ch/143793/ info:eu-repo/semantics/openAccess Sori, Michael M.; Bapst, Jonathan; Becerra, Patricio; Byrne, Shane (2019). Islands of ice on Mars and Pluto. Journal of Geophysical Research: Planets, 124(10), pp. 2522-2542. Wiley 10.1029/2018JE005861 <http://dx.doi.org/10.1029/2018JE005861> 520 Astronomy 620 Engineering info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion PeerReviewed 2019 ftunivbern https://doi.org/10.1029/2018JE005861 2023-07-31T21:59:57Z Ice sheets, such as the polar layered deposits (PLDs) of Mars, are of great interest as records of past climate. Smaller outlier ice deposits near the north and south PLDs are likely more sensitive to climate changes and thus may hold information about more recent climate history. However, the southern outlier deposits have largely remained unmapped and unanalyzed. Here, we identify 31 deposits near, but separated from, Mars's south PLDs, all of which are located within impact craters >15 km in diameter. On the basis of morphology, radar analysis, physical similarity to portions of the PLD margin, and overall similarity to previously described deposits in Mars's north polar region, we conclude that these deposits are primarily composed of water ice. An additional 66 craters contain smaller depositional features, some of which may be remnant ice deposits. The 31 outlier ice deposits represent a previously unquantified inventory of water on Mars, with a total volume between 15,000 and 38,000 km3. In addition, we identify five analogous outlier nitrogen ice deposits located within impact craters near Sputnik Planitia, the large nitrogen ice sheet on Pluto. Although important differences exist between Mars and Pluto, broad physical similarities between the two cases suggest that the topography and microclimates of impact craters cause them to be favorable locations for volatile accumulation and/or retention throughout the Solar System. Article in Journal/Newspaper Ice Sheet BORIS (Bern Open Repository and Information System, University of Bern) Sputnik ENVELOPE(66.167,66.167,-70.833,-70.833) Journal of Geophysical Research: Planets 124 10 2522 2542 |
institution |
Open Polar |
collection |
BORIS (Bern Open Repository and Information System, University of Bern) |
op_collection_id |
ftunivbern |
language |
English |
topic |
520 Astronomy 620 Engineering |
spellingShingle |
520 Astronomy 620 Engineering Sori, Michael M. Bapst, Jonathan Becerra, Patricio Byrne, Shane Islands of ice on Mars and Pluto |
topic_facet |
520 Astronomy 620 Engineering |
description |
Ice sheets, such as the polar layered deposits (PLDs) of Mars, are of great interest as records of past climate. Smaller outlier ice deposits near the north and south PLDs are likely more sensitive to climate changes and thus may hold information about more recent climate history. However, the southern outlier deposits have largely remained unmapped and unanalyzed. Here, we identify 31 deposits near, but separated from, Mars's south PLDs, all of which are located within impact craters >15 km in diameter. On the basis of morphology, radar analysis, physical similarity to portions of the PLD margin, and overall similarity to previously described deposits in Mars's north polar region, we conclude that these deposits are primarily composed of water ice. An additional 66 craters contain smaller depositional features, some of which may be remnant ice deposits. The 31 outlier ice deposits represent a previously unquantified inventory of water on Mars, with a total volume between 15,000 and 38,000 km3. In addition, we identify five analogous outlier nitrogen ice deposits located within impact craters near Sputnik Planitia, the large nitrogen ice sheet on Pluto. Although important differences exist between Mars and Pluto, broad physical similarities between the two cases suggest that the topography and microclimates of impact craters cause them to be favorable locations for volatile accumulation and/or retention throughout the Solar System. |
format |
Article in Journal/Newspaper |
author |
Sori, Michael M. Bapst, Jonathan Becerra, Patricio Byrne, Shane |
author_facet |
Sori, Michael M. Bapst, Jonathan Becerra, Patricio Byrne, Shane |
author_sort |
Sori, Michael M. |
title |
Islands of ice on Mars and Pluto |
title_short |
Islands of ice on Mars and Pluto |
title_full |
Islands of ice on Mars and Pluto |
title_fullStr |
Islands of ice on Mars and Pluto |
title_full_unstemmed |
Islands of ice on Mars and Pluto |
title_sort |
islands of ice on mars and pluto |
publisher |
Wiley |
publishDate |
2019 |
url |
https://boris.unibe.ch/143793/1/2018JE005861.pdf https://boris.unibe.ch/143793/ |
long_lat |
ENVELOPE(66.167,66.167,-70.833,-70.833) |
geographic |
Sputnik |
geographic_facet |
Sputnik |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
Sori, Michael M.; Bapst, Jonathan; Becerra, Patricio; Byrne, Shane (2019). Islands of ice on Mars and Pluto. Journal of Geophysical Research: Planets, 124(10), pp. 2522-2542. Wiley 10.1029/2018JE005861 <http://dx.doi.org/10.1029/2018JE005861> |
op_relation |
https://boris.unibe.ch/143793/ |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1029/2018JE005861 |
container_title |
Journal of Geophysical Research: Planets |
container_volume |
124 |
container_issue |
10 |
container_start_page |
2522 |
op_container_end_page |
2542 |
_version_ |
1774718766615101440 |