Non-linear flow modelling of a Martian Lobate Debris Apron

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 informati...

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Published in:Journal of Glaciology
Main Authors: Louise Steffensen Schmidt, Christine Schøtt Hvidberg, Jung Rack Kim, Nanna Bjørnholt Karlsson
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2019
Subjects:
Online Access:https://doi.org/10.1017/jog.2019.54
https://doaj.org/article/1f67cff02e624e53a94f126ffe68e017
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spelling ftdoajarticles:oai:doaj.org/article:1f67cff02e624e53a94f126ffe68e017 2023-05-15T16:57:34+02:00 Non-linear flow modelling of a Martian Lobate Debris Apron Louise Steffensen Schmidt Christine Schøtt Hvidberg Jung Rack Kim Nanna Bjørnholt Karlsson 2019-12-01T00:00:00Z https://doi.org/10.1017/jog.2019.54 https://doaj.org/article/1f67cff02e624e53a94f126ffe68e017 EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143019000546/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2019.54 0022-1430 1727-5652 https://doaj.org/article/1f67cff02e624e53a94f126ffe68e017 Journal of Glaciology, Vol 65, Pp 889-899 (2019) Extraterrestrial glaciology glacier flow glacier mass balance glacier modelling ice temperature Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2019 ftdoajarticles https://doi.org/10.1017/jog.2019.54 2023-03-12T01:30:57Z 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 Directory of Open Access Journals: DOAJ Articles Journal of Glaciology 65 254 889 899
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Extraterrestrial glaciology
glacier flow
glacier mass balance
glacier modelling
ice temperature
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
spellingShingle Extraterrestrial glaciology
glacier flow
glacier mass balance
glacier modelling
ice temperature
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
Louise Steffensen Schmidt
Christine Schøtt Hvidberg
Jung Rack Kim
Nanna Bjørnholt Karlsson
Non-linear flow modelling of a Martian Lobate Debris Apron
topic_facet Extraterrestrial glaciology
glacier flow
glacier mass balance
glacier modelling
ice temperature
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
description 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 Louise Steffensen Schmidt
Christine Schøtt Hvidberg
Jung Rack Kim
Nanna Bjørnholt Karlsson
author_facet Louise Steffensen Schmidt
Christine Schøtt Hvidberg
Jung Rack Kim
Nanna Bjørnholt Karlsson
author_sort Louise Steffensen Schmidt
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
publishDate 2019
url https://doi.org/10.1017/jog.2019.54
https://doaj.org/article/1f67cff02e624e53a94f126ffe68e017
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology, Vol 65, Pp 889-899 (2019)
op_relation https://www.cambridge.org/core/product/identifier/S0022143019000546/type/journal_article
https://doaj.org/toc/0022-1430
https://doaj.org/toc/1727-5652
doi:10.1017/jog.2019.54
0022-1430
1727-5652
https://doaj.org/article/1f67cff02e624e53a94f126ffe68e017
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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