Grounding line migration as response on periodic basal sliding pertubation

This thesis presents results of the response of an artificial ice sheet-ice shelf system to sliding pertubations concerning the grounding line migration. For that subsequent periodic basal slid- ing pertubations are applied on different time scales and geometries using the finite difference full-Sto...

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Main Author: Nieschlag, Moritz
Format: Thesis
Language:unknown
Published: 2014
Subjects:
Online Access:https://epic.awi.de/id/eprint/42346/
https://hdl.handle.net/10013/epic.49802
id ftawi:oai:epic.awi.de:42346
record_format openpolar
spelling ftawi:oai:epic.awi.de:42346 2024-09-15T18:12:32+00:00 Grounding line migration as response on periodic basal sliding pertubation Nieschlag, Moritz 2014-03 https://epic.awi.de/id/eprint/42346/ https://hdl.handle.net/10013/epic.49802 unknown Nieschlag, M. (2014) Grounding line migration as response on periodic basal sliding pertubation Master thesis, University of Hamburg. hdl:10013/epic.49802 EPIC3 Thesis notRev 2014 ftawi 2024-06-24T04:15:36Z This thesis presents results of the response of an artificial ice sheet-ice shelf system to sliding pertubations concerning the grounding line migration. For that subsequent periodic basal slid- ing pertubations are applied on different time scales and geometries using the finite difference full-Stokes model TIM-FD3 . All experiments are performed on a fixed grid. To obtain steady state geometries for the periodic sliding experiments various initial geometries including simple slabs and idealised ones are tested with horizontal resolutions from 10.0, 5.0, 2.5 to 1.25 km to investigate resolution dependencies. The pertubations experiments are examined with three geometries obtained from the geometry spin-up in comparison to applied pertubations on the geometry given by the high-resolution ice model Elmer/Ice. Most pertubation experiments are executed with a grid resolution of 2.5 km and only some with 1.25 km due to computational expenses. The experiments are a continuation of the ice2sea MISMIP3D benchmark puplished by Pat- tyn et al. (2013) at which TIM-FD3 participated. Comparability is given as the geometry of Elmer/Ice was also used for MISMIP3D. Results of the basal sliding experiments indicate that not all experiments show neutral equilib- riums in subsequent basal sliding pertubations. Thus, the grounding line migrates downstream or upstream depending on the position in comparison to the grouding line of Elmer/Ice which appears to be reversible on all resolutions and pertubations. Furthermore the tested steady state geometries show a strong dependency on the horizontal resolution and the chosen initial geometry. They do not converge to the same steady state. This strengthens the importance of the initial geometry for further pertubation experiments. Thesis Ice Sheet Ice Shelf Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
institution Open Polar
collection Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
op_collection_id ftawi
language unknown
description This thesis presents results of the response of an artificial ice sheet-ice shelf system to sliding pertubations concerning the grounding line migration. For that subsequent periodic basal slid- ing pertubations are applied on different time scales and geometries using the finite difference full-Stokes model TIM-FD3 . All experiments are performed on a fixed grid. To obtain steady state geometries for the periodic sliding experiments various initial geometries including simple slabs and idealised ones are tested with horizontal resolutions from 10.0, 5.0, 2.5 to 1.25 km to investigate resolution dependencies. The pertubations experiments are examined with three geometries obtained from the geometry spin-up in comparison to applied pertubations on the geometry given by the high-resolution ice model Elmer/Ice. Most pertubation experiments are executed with a grid resolution of 2.5 km and only some with 1.25 km due to computational expenses. The experiments are a continuation of the ice2sea MISMIP3D benchmark puplished by Pat- tyn et al. (2013) at which TIM-FD3 participated. Comparability is given as the geometry of Elmer/Ice was also used for MISMIP3D. Results of the basal sliding experiments indicate that not all experiments show neutral equilib- riums in subsequent basal sliding pertubations. Thus, the grounding line migrates downstream or upstream depending on the position in comparison to the grouding line of Elmer/Ice which appears to be reversible on all resolutions and pertubations. Furthermore the tested steady state geometries show a strong dependency on the horizontal resolution and the chosen initial geometry. They do not converge to the same steady state. This strengthens the importance of the initial geometry for further pertubation experiments.
format Thesis
author Nieschlag, Moritz
spellingShingle Nieschlag, Moritz
Grounding line migration as response on periodic basal sliding pertubation
author_facet Nieschlag, Moritz
author_sort Nieschlag, Moritz
title Grounding line migration as response on periodic basal sliding pertubation
title_short Grounding line migration as response on periodic basal sliding pertubation
title_full Grounding line migration as response on periodic basal sliding pertubation
title_fullStr Grounding line migration as response on periodic basal sliding pertubation
title_full_unstemmed Grounding line migration as response on periodic basal sliding pertubation
title_sort grounding line migration as response on periodic basal sliding pertubation
publishDate 2014
url https://epic.awi.de/id/eprint/42346/
https://hdl.handle.net/10013/epic.49802
genre Ice Sheet
Ice Shelf
genre_facet Ice Sheet
Ice Shelf
op_source EPIC3
op_relation Nieschlag, M. (2014) Grounding line migration as response on periodic basal sliding pertubation Master thesis, University of Hamburg. hdl:10013/epic.49802
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