Non-linear flow modelling of a Martian Lobate Debris Apron

Abstract The Martian mid-latitudes contain numerous small water-ice deposits, collectively termed viscous flow features (VFFs). The shape and topography of the deposits contain information on their past flow history and formation process. In order to access this information, it is imperative to get...

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Published in:Journal of Glaciology
Main Authors: Schmidt, Louise Steffensen, Hvidberg, Christine Schøtt, Kim, Jung Rack, Karlsson, Nanna Bjørnholt
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2019
Subjects:
Online Access:http://dx.doi.org/10.1017/jog.2019.54
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143019000546
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spelling crcambridgeupr:10.1017/jog.2019.54 2024-03-03T08:46:02+00:00 Non-linear flow modelling of a Martian Lobate Debris Apron Schmidt, Louise Steffensen Hvidberg, Christine Schøtt Kim, Jung Rack Karlsson, Nanna Bjørnholt 2019 http://dx.doi.org/10.1017/jog.2019.54 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143019000546 en eng Cambridge University Press (CUP) http://creativecommons.org/licenses/by/4.0/ Journal of Glaciology volume 65, issue 254, page 889-899 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 2019 crcambridgeupr https://doi.org/10.1017/jog.2019.54 2024-02-08T08:43:06Z Abstract The Martian mid-latitudes contain numerous small water-ice deposits, collectively termed viscous flow features (VFFs). The shape and topography of the deposits contain information on their past flow history and formation process. In order to access this information, it is imperative to get information on their deformational properties. Here we use a high-resolution digital topography map and ice-penetrating radar data in combination with an inverse method to constrain the deformational properties of a lobate debris apron, a class of VFF, in the southern hemisphere of Mars. We find that while the creep parameter and accumulation rates are not well constrained in absolute values, their ratio is robust. We also find that the creep exponent is most likely n ≤ 3. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 65 254 889 899
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Schmidt, Louise Steffensen
Hvidberg, Christine Schøtt
Kim, Jung Rack
Karlsson, Nanna Bjørnholt
Non-linear flow modelling of a Martian Lobate Debris Apron
topic_facet Earth-Surface Processes
description Abstract The Martian mid-latitudes contain numerous small water-ice deposits, collectively termed viscous flow features (VFFs). The shape and topography of the deposits contain information on their past flow history and formation process. In order to access this information, it is imperative to get information on their deformational properties. Here we use a high-resolution digital topography map and ice-penetrating radar data in combination with an inverse method to constrain the deformational properties of a lobate debris apron, a class of VFF, in the southern hemisphere of Mars. We find that while the creep parameter and accumulation rates are not well constrained in absolute values, their ratio is robust. We also find that the creep exponent is most likely n ≤ 3.
format Article in Journal/Newspaper
author Schmidt, Louise Steffensen
Hvidberg, Christine Schøtt
Kim, Jung Rack
Karlsson, Nanna Bjørnholt
author_facet Schmidt, Louise Steffensen
Hvidberg, Christine Schøtt
Kim, Jung Rack
Karlsson, Nanna Bjørnholt
author_sort Schmidt, Louise Steffensen
title Non-linear flow modelling of a Martian Lobate Debris Apron
title_short Non-linear flow modelling of a Martian Lobate Debris Apron
title_full Non-linear flow modelling of a Martian Lobate Debris Apron
title_fullStr Non-linear flow modelling of a Martian Lobate Debris Apron
title_full_unstemmed Non-linear flow modelling of a Martian Lobate Debris Apron
title_sort non-linear flow modelling of a martian lobate debris apron
publisher Cambridge University Press (CUP)
publishDate 2019
url http://dx.doi.org/10.1017/jog.2019.54
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143019000546
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 65, issue 254, page 889-899
ISSN 0022-1430 1727-5652
op_rights http://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1017/jog.2019.54
container_title Journal of Glaciology
container_volume 65
container_issue 254
container_start_page 889
op_container_end_page 899
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