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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Lancaster University
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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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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 |
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Lancaster University: Lancaster Eprints |
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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 |
_version_ |
1799480330987503616 |