Improving Ice Sheet Model Calibration Using Paleoclimate and Modern Data

Human-induced climate change may cause significant ice volume loss from the West Antarctic Ice Sheet (WAIS). Projections of ice volume change from ice-sheet models and corresponding future sea-level rise have large uncertainties due to poorly constrained input parameters. In most future applications...

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Main Authors: Chang, Won, Haran, Murali, Applegate, Patrick, Pollard, David
Format: Text
Language:unknown
Published: arXiv 2015
Subjects:
Online Access:https://dx.doi.org/10.48550/arxiv.1510.01676
https://arxiv.org/abs/1510.01676
id ftdatacite:10.48550/arxiv.1510.01676
record_format openpolar
spelling ftdatacite:10.48550/arxiv.1510.01676 2023-05-15T13:46:05+02:00 Improving Ice Sheet Model Calibration Using Paleoclimate and Modern Data Chang, Won Haran, Murali Applegate, Patrick Pollard, David 2015 https://dx.doi.org/10.48550/arxiv.1510.01676 https://arxiv.org/abs/1510.01676 unknown arXiv arXiv.org perpetual, non-exclusive license http://arxiv.org/licenses/nonexclusive-distrib/1.0/ Applications stat.AP FOS Computer and information sciences article-journal Article ScholarlyArticle Text 2015 ftdatacite https://doi.org/10.48550/arxiv.1510.01676 2022-04-01T12:11:25Z Human-induced climate change may cause significant ice volume loss from the West Antarctic Ice Sheet (WAIS). Projections of ice volume change from ice-sheet models and corresponding future sea-level rise have large uncertainties due to poorly constrained input parameters. In most future applications to date, model calibration has utilized only modern or recent (decadal) observations, leaving input parameters that control the long-term behavior of WAIS largely unconstrained. Many paleo-observations are in the form of localized time series, while modern observations are non-Gaussian spatial data; combining information across these types poses non-trivial statistical challenges. Here we introduce a computationally efficient calibration approach that utilizes both modern and paleo-observations to generate better-constrained ice volume projections. Using fast emulators built upon principal component analysis and a reduced dimension calibration model, we can efficiently handle high-dimensional and non-Gaussian data. We apply our calibration approach to the PSU3D-ICE model which can realistically simulate long-term behavior of WAIS. Our results show that using paleo observations in calibration significantly reduces parametric uncertainty, resulting in sharper projections about the future state of WAIS. One benefit of using paleo observations is found to be that unrealistic simulations with overshoots in past ice retreat and projected future regrowth are eliminated. Text Antarc* Antarctic Ice Sheet DataCite Metadata Store (German National Library of Science and Technology) Antarctic West Antarctic Ice Sheet
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic Applications stat.AP
FOS Computer and information sciences
spellingShingle Applications stat.AP
FOS Computer and information sciences
Chang, Won
Haran, Murali
Applegate, Patrick
Pollard, David
Improving Ice Sheet Model Calibration Using Paleoclimate and Modern Data
topic_facet Applications stat.AP
FOS Computer and information sciences
description Human-induced climate change may cause significant ice volume loss from the West Antarctic Ice Sheet (WAIS). Projections of ice volume change from ice-sheet models and corresponding future sea-level rise have large uncertainties due to poorly constrained input parameters. In most future applications to date, model calibration has utilized only modern or recent (decadal) observations, leaving input parameters that control the long-term behavior of WAIS largely unconstrained. Many paleo-observations are in the form of localized time series, while modern observations are non-Gaussian spatial data; combining information across these types poses non-trivial statistical challenges. Here we introduce a computationally efficient calibration approach that utilizes both modern and paleo-observations to generate better-constrained ice volume projections. Using fast emulators built upon principal component analysis and a reduced dimension calibration model, we can efficiently handle high-dimensional and non-Gaussian data. We apply our calibration approach to the PSU3D-ICE model which can realistically simulate long-term behavior of WAIS. Our results show that using paleo observations in calibration significantly reduces parametric uncertainty, resulting in sharper projections about the future state of WAIS. One benefit of using paleo observations is found to be that unrealistic simulations with overshoots in past ice retreat and projected future regrowth are eliminated.
format Text
author Chang, Won
Haran, Murali
Applegate, Patrick
Pollard, David
author_facet Chang, Won
Haran, Murali
Applegate, Patrick
Pollard, David
author_sort Chang, Won
title Improving Ice Sheet Model Calibration Using Paleoclimate and Modern Data
title_short Improving Ice Sheet Model Calibration Using Paleoclimate and Modern Data
title_full Improving Ice Sheet Model Calibration Using Paleoclimate and Modern Data
title_fullStr Improving Ice Sheet Model Calibration Using Paleoclimate and Modern Data
title_full_unstemmed Improving Ice Sheet Model Calibration Using Paleoclimate and Modern Data
title_sort improving ice sheet model calibration using paleoclimate and modern data
publisher arXiv
publishDate 2015
url https://dx.doi.org/10.48550/arxiv.1510.01676
https://arxiv.org/abs/1510.01676
geographic Antarctic
West Antarctic Ice Sheet
geographic_facet Antarctic
West Antarctic Ice Sheet
genre Antarc*
Antarctic
Ice Sheet
genre_facet Antarc*
Antarctic
Ice Sheet
op_rights arXiv.org perpetual, non-exclusive license
http://arxiv.org/licenses/nonexclusive-distrib/1.0/
op_doi https://doi.org/10.48550/arxiv.1510.01676
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