The State and Future of Mars Polar Science and Exploration
As the planet's principal cold traps, the martian polar regions have accumulated extensive mantles of ice and dust that cover individual areas of ∼10^6 km^2 and total as much as 3–4 km thick. From the scarcity of superposed craters on their surface, these layered deposits are thought to be comp...
Published in: | Icarus |
---|---|
Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
Elsevier
2000
|
Subjects: | |
Online Access: | https://authors.library.caltech.edu/36559/ https://resolver.caltech.edu/CaltechAUTHORS:20130124-090538648 |
id |
ftcaltechauth:oai:authors.library.caltech.edu:36559 |
---|---|
record_format |
openpolar |
spelling |
ftcaltechauth:oai:authors.library.caltech.edu:36559 2023-05-15T18:02:49+02:00 The State and Future of Mars Polar Science and Exploration Clifford, Stephen M. Ingersoll, Andy P. Murray, Bruce 2000-04 https://authors.library.caltech.edu/36559/ https://resolver.caltech.edu/CaltechAUTHORS:20130124-090538648 unknown Elsevier Clifford, Stephen M. and Ingersoll, Andy P. and Murray, Bruce (2000) The State and Future of Mars Polar Science and Exploration. Icarus, 144 (2). pp. 210-242. ISSN 0019-1035. doi:10.1006/icar.1999.6290. https://resolver.caltech.edu/CaltechAUTHORS:20130124-090538648 <https://resolver.caltech.edu/CaltechAUTHORS:20130124-090538648> Article PeerReviewed 2000 ftcaltechauth https://doi.org/10.1006/icar.1999.6290 2021-11-11T18:52:36Z As the planet's principal cold traps, the martian polar regions have accumulated extensive mantles of ice and dust that cover individual areas of ∼10^6 km^2 and total as much as 3–4 km thick. From the scarcity of superposed craters on their surface, these layered deposits are thought to be comparatively young—preserving a record of the seasonal and climatic cycling of atmospheric CO_2, H_2O, and dust over the past ∼10^5–10^8 years. For this reason, the martian polar deposits may serve as a Rosetta Stone for understanding the geologic and climatic history of the planet—documenting variations in insolation (due to quasiperiodic oscillations in the planet's obliquity and orbital elements), volatile mass balance, atmospheric composition, dust storm activity, volcanic eruptions, large impacts, catastrophic floods, solar luminosity, supernovae, and perhaps even a record of microbial life. Beyond their scientific value, the polar regions may soon prove important for another reason—providing a valuable and accessible reservoir of water to support the long-term human exploration of Mars. In this paper we assess the current state of Mars polar research, identify the key questions that motivate the exploration of the polar regions, discuss the extent to which current missions will address these questions, and speculate about what additional capabilities and investigations may be required to address the issues that remain outstanding. Article in Journal/Newspaper Polar Science Caltech Authors (California Institute of Technology) Icarus 144 2 210 242 |
institution |
Open Polar |
collection |
Caltech Authors (California Institute of Technology) |
op_collection_id |
ftcaltechauth |
language |
unknown |
description |
As the planet's principal cold traps, the martian polar regions have accumulated extensive mantles of ice and dust that cover individual areas of ∼10^6 km^2 and total as much as 3–4 km thick. From the scarcity of superposed craters on their surface, these layered deposits are thought to be comparatively young—preserving a record of the seasonal and climatic cycling of atmospheric CO_2, H_2O, and dust over the past ∼10^5–10^8 years. For this reason, the martian polar deposits may serve as a Rosetta Stone for understanding the geologic and climatic history of the planet—documenting variations in insolation (due to quasiperiodic oscillations in the planet's obliquity and orbital elements), volatile mass balance, atmospheric composition, dust storm activity, volcanic eruptions, large impacts, catastrophic floods, solar luminosity, supernovae, and perhaps even a record of microbial life. Beyond their scientific value, the polar regions may soon prove important for another reason—providing a valuable and accessible reservoir of water to support the long-term human exploration of Mars. In this paper we assess the current state of Mars polar research, identify the key questions that motivate the exploration of the polar regions, discuss the extent to which current missions will address these questions, and speculate about what additional capabilities and investigations may be required to address the issues that remain outstanding. |
format |
Article in Journal/Newspaper |
author |
Clifford, Stephen M. Ingersoll, Andy P. Murray, Bruce |
spellingShingle |
Clifford, Stephen M. Ingersoll, Andy P. Murray, Bruce The State and Future of Mars Polar Science and Exploration |
author_facet |
Clifford, Stephen M. Ingersoll, Andy P. Murray, Bruce |
author_sort |
Clifford, Stephen M. |
title |
The State and Future of Mars Polar Science and Exploration |
title_short |
The State and Future of Mars Polar Science and Exploration |
title_full |
The State and Future of Mars Polar Science and Exploration |
title_fullStr |
The State and Future of Mars Polar Science and Exploration |
title_full_unstemmed |
The State and Future of Mars Polar Science and Exploration |
title_sort |
state and future of mars polar science and exploration |
publisher |
Elsevier |
publishDate |
2000 |
url |
https://authors.library.caltech.edu/36559/ https://resolver.caltech.edu/CaltechAUTHORS:20130124-090538648 |
genre |
Polar Science |
genre_facet |
Polar Science |
op_relation |
Clifford, Stephen M. and Ingersoll, Andy P. and Murray, Bruce (2000) The State and Future of Mars Polar Science and Exploration. Icarus, 144 (2). pp. 210-242. ISSN 0019-1035. doi:10.1006/icar.1999.6290. https://resolver.caltech.edu/CaltechAUTHORS:20130124-090538648 <https://resolver.caltech.edu/CaltechAUTHORS:20130124-090538648> |
op_doi |
https://doi.org/10.1006/icar.1999.6290 |
container_title |
Icarus |
container_volume |
144 |
container_issue |
2 |
container_start_page |
210 |
op_container_end_page |
242 |
_version_ |
1766173472477675520 |