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...

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Published in:Icarus
Main Authors: Clifford, Stephen M., Ingersoll, Andy P., Murray, Bruce
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
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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
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