Fibre-optic borehole observations and numerical modelling of complex ice-sheet thermodynamics ...

Predictions of ice-sheet mass loss, and therefore predictions of global sea level rise, depend sensitively upon how ice-sheet motion is incorporated into numerical models. Using field observations and numerical modelling, this thesis demonstrates that two frequently overlooked processes are central...

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Bibliographic Details
Main Author: Law, Robert
Format: Thesis
Language:English
Published: Apollo - University of Cambridge Repository 2022
Subjects:
Online Access:https://dx.doi.org/10.17863/cam.90692
https://www.repository.cam.ac.uk/handle/1810/343281
id ftdatacite:10.17863/cam.90692
record_format openpolar
spelling ftdatacite:10.17863/cam.90692 2024-02-04T09:56:04+01:00 Fibre-optic borehole observations and numerical modelling of complex ice-sheet thermodynamics ... Law, Robert 2022 https://dx.doi.org/10.17863/cam.90692 https://www.repository.cam.ac.uk/handle/1810/343281 en eng Apollo - University of Cambridge Repository https://dx.doi.org/10.17863/cam.65812 open.access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 http://purl.org/coar/access_right/c_abf2 Antarctic Ice Sheet Fibre-optics Finite Element Modelling Glacier borehole Glacier fieldwork Glaciology Greenland Ice Sheet Dissertation Thesis thesis 2022 ftdatacite https://doi.org/10.17863/cam.9069210.17863/cam.65812 2024-01-05T09:50:49Z Predictions of ice-sheet mass loss, and therefore predictions of global sea level rise, depend sensitively upon how ice-sheet motion is incorporated into numerical models. Using field observations and numerical modelling, this thesis demonstrates that two frequently overlooked processes are central to describing borehole observations of fast ice-sheet motion --- intermediate-scale (<25 m, ⪅2 km) interaction of ice motion with realistic or real bed topography, and modulation of these ice-motion patterns through a basal layer of temperate ice (much softer ice at the pressure-melting point). I first present a fibre-optic data set from a 1,043 m deep borehole drilled to the base of the fast-moving (>500 m a‾¹) marine-terminating Sermeq Kujalleq (Store Glacier) at the western margin of the Greenland Ice Sheet. This reveals hitherto unappreciated complexity in the processes behind fast ice-sheet motion. I observe substantial but isolated strain heating ~220 m beneath the surface within stiffer ... Thesis Antarc* Antarctic glacier Greenland Ice Sheet Kujalleq Sermeq Kujalleq DataCite Metadata Store (German National Library of Science and Technology) Antarctic Greenland Kujalleq ENVELOPE(-46.037,-46.037,60.719,60.719)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Antarctic Ice Sheet
Fibre-optics
Finite Element Modelling
Glacier borehole
Glacier fieldwork
Glaciology
Greenland Ice Sheet
spellingShingle Antarctic Ice Sheet
Fibre-optics
Finite Element Modelling
Glacier borehole
Glacier fieldwork
Glaciology
Greenland Ice Sheet
Law, Robert
Fibre-optic borehole observations and numerical modelling of complex ice-sheet thermodynamics ...
topic_facet Antarctic Ice Sheet
Fibre-optics
Finite Element Modelling
Glacier borehole
Glacier fieldwork
Glaciology
Greenland Ice Sheet
description Predictions of ice-sheet mass loss, and therefore predictions of global sea level rise, depend sensitively upon how ice-sheet motion is incorporated into numerical models. Using field observations and numerical modelling, this thesis demonstrates that two frequently overlooked processes are central to describing borehole observations of fast ice-sheet motion --- intermediate-scale (<25 m, ⪅2 km) interaction of ice motion with realistic or real bed topography, and modulation of these ice-motion patterns through a basal layer of temperate ice (much softer ice at the pressure-melting point). I first present a fibre-optic data set from a 1,043 m deep borehole drilled to the base of the fast-moving (>500 m a‾¹) marine-terminating Sermeq Kujalleq (Store Glacier) at the western margin of the Greenland Ice Sheet. This reveals hitherto unappreciated complexity in the processes behind fast ice-sheet motion. I observe substantial but isolated strain heating ~220 m beneath the surface within stiffer ...
format Thesis
author Law, Robert
author_facet Law, Robert
author_sort Law, Robert
title Fibre-optic borehole observations and numerical modelling of complex ice-sheet thermodynamics ...
title_short Fibre-optic borehole observations and numerical modelling of complex ice-sheet thermodynamics ...
title_full Fibre-optic borehole observations and numerical modelling of complex ice-sheet thermodynamics ...
title_fullStr Fibre-optic borehole observations and numerical modelling of complex ice-sheet thermodynamics ...
title_full_unstemmed Fibre-optic borehole observations and numerical modelling of complex ice-sheet thermodynamics ...
title_sort fibre-optic borehole observations and numerical modelling of complex ice-sheet thermodynamics ...
publisher Apollo - University of Cambridge Repository
publishDate 2022
url https://dx.doi.org/10.17863/cam.90692
https://www.repository.cam.ac.uk/handle/1810/343281
long_lat ENVELOPE(-46.037,-46.037,60.719,60.719)
geographic Antarctic
Greenland
Kujalleq
geographic_facet Antarctic
Greenland
Kujalleq
genre Antarc*
Antarctic
glacier
Greenland
Ice Sheet
Kujalleq
Sermeq Kujalleq
genre_facet Antarc*
Antarctic
glacier
Greenland
Ice Sheet
Kujalleq
Sermeq Kujalleq
op_relation https://dx.doi.org/10.17863/cam.65812
op_rights open.access
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
http://purl.org/coar/access_right/c_abf2
op_doi https://doi.org/10.17863/cam.9069210.17863/cam.65812
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