Addressing uncertainty in firn densification models for applications on the Greenland and Antarctic ice sheets.

Ice sheets form from snow which has been compacted into ice over many years. As snow transitions into ice, it passes through an intermediate stage known as firn. Both the Greenland and Antarctic ice sheets are covered by a firn layer that can be up to ~150 m thick, with lighter firn closer to the su...

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Main Authors: Verjans, Vincent, Leeson, Amber, McMillan, Mal, Beven, Keith
Format: Thesis
Language:English
Published: Lancaster University 2021
Subjects:
Online Access:https://eprints.lancs.ac.uk/id/eprint/154254/
https://eprints.lancs.ac.uk/id/eprint/154254/1/2021Verjansphd.pdf
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spelling ftulancaster:oai:eprints.lancs.ac.uk:154254 2024-05-19T07:29:37+00:00 Addressing uncertainty in firn densification models for applications on the Greenland and Antarctic ice sheets. Verjans, Vincent Leeson, Amber McMillan, Mal Beven, Keith 2021 text https://eprints.lancs.ac.uk/id/eprint/154254/ https://eprints.lancs.ac.uk/id/eprint/154254/1/2021Verjansphd.pdf en eng Lancaster University https://eprints.lancs.ac.uk/id/eprint/154254/1/2021Verjansphd.pdf Verjans, Vincent and Leeson, Amber and McMillan, Mal and Beven, Keith (2021) Addressing uncertainty in firn densification models for applications on the Greenland and Antarctic ice sheets. PhD thesis, Lancaster Environment Centre. creative_commons_attribution_4_0_international_license Thesis NonPeerReviewed 2021 ftulancaster 2024-04-30T23:37:14Z Ice sheets form from snow which has been compacted into ice over many years. As snow transitions into ice, it passes through an intermediate stage known as firn. Both the Greenland and Antarctic ice sheets are covered by a firn layer that can be up to ~150 m thick, with lighter firn closer to the surface and denser firn at depth. Firn models aim at representing densification processes as a function of climate (e.g. snowfall and temperature), and model simulations can be performed on large spatial scales, e.g. for ice sheet mass balance assessments, or at individual locations, e.g. for analyses of ice cores. Firn densification models are empirical models, thus relying on calibration with observational data. In this context, there are several sources of inter-model discrepancies: calibration methodology, calibration data, level of model complexity, physical processes included and their parameterisation, and climatic input forcing. For all these reasons, uncertainty about firn densification results is large, yet difficult to evaluate. This thesis aims to better quantify uncertainty from these aspects, and their impact on firn model output. In Chapter 1, a new model implementation for simulating meltwater percolation in firn models is presented and evaluated. Representing meltwater infiltration and the subsequent effects on firn densification and temperature properties remains a primary source of uncertainty in firn models. This study provides a novel and physics-based approach to represent the meltwater flow process and its interplay with firn densification. Uncertainty associated with model parameterisation and with the calibration process is addressed in Chapter 2. Using a large dataset of firn cores, a Bayesian calibration framework is designed and used in order to re-estimate model parameter values. This statistical approach further allows to quantify parametric uncertainties and their direct impact on modelled densification rates. Chapter 3 is the first study to thoroughly evaluate uncertainty in firn ... Thesis Antarc* Antarctic Greenland Ice Sheet Lancaster University: Lancaster Eprints
institution Open Polar
collection Lancaster University: Lancaster Eprints
op_collection_id ftulancaster
language English
description Ice sheets form from snow which has been compacted into ice over many years. As snow transitions into ice, it passes through an intermediate stage known as firn. Both the Greenland and Antarctic ice sheets are covered by a firn layer that can be up to ~150 m thick, with lighter firn closer to the surface and denser firn at depth. Firn models aim at representing densification processes as a function of climate (e.g. snowfall and temperature), and model simulations can be performed on large spatial scales, e.g. for ice sheet mass balance assessments, or at individual locations, e.g. for analyses of ice cores. Firn densification models are empirical models, thus relying on calibration with observational data. In this context, there are several sources of inter-model discrepancies: calibration methodology, calibration data, level of model complexity, physical processes included and their parameterisation, and climatic input forcing. For all these reasons, uncertainty about firn densification results is large, yet difficult to evaluate. This thesis aims to better quantify uncertainty from these aspects, and their impact on firn model output. In Chapter 1, a new model implementation for simulating meltwater percolation in firn models is presented and evaluated. Representing meltwater infiltration and the subsequent effects on firn densification and temperature properties remains a primary source of uncertainty in firn models. This study provides a novel and physics-based approach to represent the meltwater flow process and its interplay with firn densification. Uncertainty associated with model parameterisation and with the calibration process is addressed in Chapter 2. Using a large dataset of firn cores, a Bayesian calibration framework is designed and used in order to re-estimate model parameter values. This statistical approach further allows to quantify parametric uncertainties and their direct impact on modelled densification rates. Chapter 3 is the first study to thoroughly evaluate uncertainty in firn ...
format Thesis
author Verjans, Vincent
Leeson, Amber
McMillan, Mal
Beven, Keith
spellingShingle Verjans, Vincent
Leeson, Amber
McMillan, Mal
Beven, Keith
Addressing uncertainty in firn densification models for applications on the Greenland and Antarctic ice sheets.
author_facet Verjans, Vincent
Leeson, Amber
McMillan, Mal
Beven, Keith
author_sort Verjans, Vincent
title Addressing uncertainty in firn densification models for applications on the Greenland and Antarctic ice sheets.
title_short Addressing uncertainty in firn densification models for applications on the Greenland and Antarctic ice sheets.
title_full Addressing uncertainty in firn densification models for applications on the Greenland and Antarctic ice sheets.
title_fullStr Addressing uncertainty in firn densification models for applications on the Greenland and Antarctic ice sheets.
title_full_unstemmed Addressing uncertainty in firn densification models for applications on the Greenland and Antarctic ice sheets.
title_sort addressing uncertainty in firn densification models for applications on the greenland and antarctic ice sheets.
publisher Lancaster University
publishDate 2021
url https://eprints.lancs.ac.uk/id/eprint/154254/
https://eprints.lancs.ac.uk/id/eprint/154254/1/2021Verjansphd.pdf
genre Antarc*
Antarctic
Greenland
Ice Sheet
genre_facet Antarc*
Antarctic
Greenland
Ice Sheet
op_relation https://eprints.lancs.ac.uk/id/eprint/154254/1/2021Verjansphd.pdf
Verjans, Vincent and Leeson, Amber and McMillan, Mal and Beven, Keith (2021) Addressing uncertainty in firn densification models for applications on the Greenland and Antarctic ice sheets. PhD thesis, Lancaster Environment Centre.
op_rights creative_commons_attribution_4_0_international_license
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