A Migration Model for the Polar Spiral Troughs of Mars
Mars' iconic polar spiral troughs are 400-1,000-m-deep depressions in the north polarlayered deposits. As the north polarlayered deposits accumulate, troughs migrate approximately poleward, anti-parallel to the local wind patterns. Insolation is suspected to drive ice retreat through sublimatio...
Published in: | Journal of Geophysical Research: Planets |
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Main Authors: | , , , , |
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Format: | Article in Journal/Newspaper |
Language: | English |
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AMER GEOPHYSICAL UNION
2019
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Subjects: | |
Online Access: | http://hdl.handle.net/10150/634775 https://doi.org/10.1029/2018je005806 |
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ftunivarizona:oai:repository.arizona.edu:10150/634775 |
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openpolar |
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Open Polar |
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The University of Arizona: UA Campus Repository |
op_collection_id |
ftunivarizona |
language |
English |
topic |
Mars ice sublimation radar planetary geomorphology |
spellingShingle |
Mars ice sublimation radar planetary geomorphology Bramson, A. M. Byrne, S. Bapst, J. Smith, I. B. McClintock, T. A Migration Model for the Polar Spiral Troughs of Mars |
topic_facet |
Mars ice sublimation radar planetary geomorphology |
description |
Mars' iconic polar spiral troughs are 400-1,000-m-deep depressions in the north polarlayered deposits. As the north polarlayered deposits accumulate, troughs migrate approximately poleward, anti-parallel to the local wind patterns. Insolation is suspected to drive ice retreat through sublimation. Sublimation at the trough wall produces a growing sublimation lag that modulates further retreat; however, winds move material off the retreating slope faces, thinning the lag. Discontinuities in stratigraphy seen by radar highlight Trough Migration Paths (TMPs), which provide a record of the troughs' position, formation, and evolution to the present day. We investigate two adjacent troughs presently near 87 degrees N to evaluate the mass balance conditions at those sites. We constrain the contribution of insolation-induced sublimation to the migration in the observed TMPs. We present a phenomenological model that combines our simulations of the sublimation conditions at paleo-trough surfaces with accumulation rates to create synthetic TMPs that are tunable to the observations. Models using nominal values of lag diffusivity, albedo, and atmospheric water vapor abundance and in which the trough walls have been covered in a lag on the order of millimeters thick and formed 2.3Myr ago match the observed trough migration and align with expectations of trough ages. Thicker lags, and/or older troughs, would generate TMPs of constant slope, which does not match the observed paths. We demonstrate the viability of our new theoretical model for predicting conditions that lead to trough migration, allowing us to connect observable TMPs to Martian climate processes. Plain Language Summary Mars' iconic polar spiral troughs are depressions in Mars' northern polar ice cap. The positions of these troughs have migrated poleward over time. Exposure to the Sun's radiation is suspected to drive retreat of the ice through sublimation (ice transitioning directly into vapor without a liquid phase). When ice sublimates, it leaves behind any dust that was within the ice, protecting the ice from further sublimation. Winds, however, have thinned this dust cover, allowing the troughs to continue migrating. Ice layering in subsurface radar data map out the migration paths of the troughs, which provide a record of the troughs' position from their formation to the present day. We investigate ice stability conditions at two adjacent troughs and present a new theoretical model for trough migration. We model sublimation of the trough walls and combine our simulations with previously proposed ice accumulation rates for Mars' north pole to create synthetic trough migration paths. In comparing our models to the observations of trough migration, we find that the trough walls have been covered in millimeters-thick dust over 2.3Myr, consistent with previously hypothesized ages. Our physical modeling approach allows us to connect the observable trough migration paths to Martian climate processes. NASA Earth and Space Sciences Fellowship (NESSF) [NNX16AP09H] 6 month embargo; published online: 23 April 2019 This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu. |
author2 |
Univ Arizona, Dept Phys Univ Arizona, Lunar & Planetary Lab |
format |
Article in Journal/Newspaper |
author |
Bramson, A. M. Byrne, S. Bapst, J. Smith, I. B. McClintock, T. |
author_facet |
Bramson, A. M. Byrne, S. Bapst, J. Smith, I. B. McClintock, T. |
author_sort |
Bramson, A. M. |
title |
A Migration Model for the Polar Spiral Troughs of Mars |
title_short |
A Migration Model for the Polar Spiral Troughs of Mars |
title_full |
A Migration Model for the Polar Spiral Troughs of Mars |
title_fullStr |
A Migration Model for the Polar Spiral Troughs of Mars |
title_full_unstemmed |
A Migration Model for the Polar Spiral Troughs of Mars |
title_sort |
migration model for the polar spiral troughs of mars |
publisher |
AMER GEOPHYSICAL UNION |
publishDate |
2019 |
url |
http://hdl.handle.net/10150/634775 https://doi.org/10.1029/2018je005806 |
geographic |
North Pole |
geographic_facet |
North Pole |
genre |
Ice cap North Pole |
genre_facet |
Ice cap North Pole |
op_source |
124 4 1020-1043 |
op_relation |
Bramson, A. M., Byrne, S., Bapst, J., Smith, I. B., & McClintock, T. (2019). A migration model for the polar spiral troughs of Mars. Journal of Geophysical Research: Planets, 124, 1020–1043. https://doi.org/10.1029/2018JE005806 2169-9097 doi:10.1029/2018je005806 http://hdl.handle.net/10150/634775 JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS |
op_rights |
Copyright © 2019. American Geophysical Union. All Rights Reserved. |
op_doi |
https://doi.org/10.1029/2018je005806 https://doi.org/10.1029/2018JE005806 |
container_title |
Journal of Geophysical Research: Planets |
container_volume |
124 |
container_issue |
4 |
container_start_page |
1020 |
op_container_end_page |
1043 |
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1766028680107130880 |
spelling |
ftunivarizona:oai:repository.arizona.edu:10150/634775 2023-05-15T16:38:25+02:00 A Migration Model for the Polar Spiral Troughs of Mars Bramson, A. M. Byrne, S. Bapst, J. Smith, I. B. McClintock, T. Univ Arizona, Dept Phys Univ Arizona, Lunar & Planetary Lab 2019-04-23 http://hdl.handle.net/10150/634775 https://doi.org/10.1029/2018je005806 en eng AMER GEOPHYSICAL UNION Bramson, A. M., Byrne, S., Bapst, J., Smith, I. B., & McClintock, T. (2019). A migration model for the polar spiral troughs of Mars. Journal of Geophysical Research: Planets, 124, 1020–1043. https://doi.org/10.1029/2018JE005806 2169-9097 doi:10.1029/2018je005806 http://hdl.handle.net/10150/634775 JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS Copyright © 2019. American Geophysical Union. All Rights Reserved. 124 4 1020-1043 Mars ice sublimation radar planetary geomorphology Article 2019 ftunivarizona https://doi.org/10.1029/2018je005806 https://doi.org/10.1029/2018JE005806 2020-06-14T08:17:58Z Mars' iconic polar spiral troughs are 400-1,000-m-deep depressions in the north polarlayered deposits. As the north polarlayered deposits accumulate, troughs migrate approximately poleward, anti-parallel to the local wind patterns. Insolation is suspected to drive ice retreat through sublimation. Sublimation at the trough wall produces a growing sublimation lag that modulates further retreat; however, winds move material off the retreating slope faces, thinning the lag. Discontinuities in stratigraphy seen by radar highlight Trough Migration Paths (TMPs), which provide a record of the troughs' position, formation, and evolution to the present day. We investigate two adjacent troughs presently near 87 degrees N to evaluate the mass balance conditions at those sites. We constrain the contribution of insolation-induced sublimation to the migration in the observed TMPs. We present a phenomenological model that combines our simulations of the sublimation conditions at paleo-trough surfaces with accumulation rates to create synthetic TMPs that are tunable to the observations. Models using nominal values of lag diffusivity, albedo, and atmospheric water vapor abundance and in which the trough walls have been covered in a lag on the order of millimeters thick and formed 2.3Myr ago match the observed trough migration and align with expectations of trough ages. Thicker lags, and/or older troughs, would generate TMPs of constant slope, which does not match the observed paths. We demonstrate the viability of our new theoretical model for predicting conditions that lead to trough migration, allowing us to connect observable TMPs to Martian climate processes. Plain Language Summary Mars' iconic polar spiral troughs are depressions in Mars' northern polar ice cap. The positions of these troughs have migrated poleward over time. Exposure to the Sun's radiation is suspected to drive retreat of the ice through sublimation (ice transitioning directly into vapor without a liquid phase). When ice sublimates, it leaves behind any dust that was within the ice, protecting the ice from further sublimation. Winds, however, have thinned this dust cover, allowing the troughs to continue migrating. Ice layering in subsurface radar data map out the migration paths of the troughs, which provide a record of the troughs' position from their formation to the present day. We investigate ice stability conditions at two adjacent troughs and present a new theoretical model for trough migration. We model sublimation of the trough walls and combine our simulations with previously proposed ice accumulation rates for Mars' north pole to create synthetic trough migration paths. In comparing our models to the observations of trough migration, we find that the trough walls have been covered in millimeters-thick dust over 2.3Myr, consistent with previously hypothesized ages. Our physical modeling approach allows us to connect the observable trough migration paths to Martian climate processes. NASA Earth and Space Sciences Fellowship (NESSF) [NNX16AP09H] 6 month embargo; published online: 23 April 2019 This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu. Article in Journal/Newspaper Ice cap North Pole The University of Arizona: UA Campus Repository North Pole Journal of Geophysical Research: Planets 124 4 1020 1043 |