Tracer transport in an isochronal ice-sheet model ...

The full history of ice sheet and climate interactions is recorded in the vertical profiles of geochemical tracers in polar ice sheets. Numerical simulations of these archives promise great advances both in the interpretation of these reconstructions and the validation of the models themselves. Howe...

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Main Author: Born, Andreas
Format: Text
Language:English
Published: International Glaciological Society 2016
Subjects:
Online Access:https://dx.doi.org/10.7892/boris.93879
http://boris.unibe.ch/93879/
id ftdatacite:10.7892/boris.93879
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spelling ftdatacite:10.7892/boris.93879 2024-09-15T18:09:44+00:00 Tracer transport in an isochronal ice-sheet model ... Born, Andreas 2016 application/pdf https://dx.doi.org/10.7892/boris.93879 http://boris.unibe.ch/93879/ en eng International Glaciological Society info:eu-repo/semantics/openAccess 530 Physics Text ScholarlyArticle article-journal 2016 ftdatacite https://doi.org/10.7892/boris.93879 2024-09-02T10:17:31Z The full history of ice sheet and climate interactions is recorded in the vertical profiles of geochemical tracers in polar ice sheets. Numerical simulations of these archives promise great advances both in the interpretation of these reconstructions and the validation of the models themselves. However, fundamental mathematical shortcomings of existing models subject tracers to spurious diffusion, thwarting straightforward solutions. Here, I propose a new vertical discretization for ice-sheet models that eliminates numerical diffusion entirely. Vertical motion through the model mesh is avoided by mimicking the real-world flow of ice as a thinning of underlying layers. A new layer is added to the surface at equidistant time intervals, isochronally, thus identifying each layer uniquely by its time of deposition and age. This new approach is implemented for a two-dimensional section through the summit of the Greenland ice sheet. The ability to directly compare simulations of vertical ice cores with ... Text Greenland Ice Sheet DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic 530 Physics
spellingShingle 530 Physics
Born, Andreas
Tracer transport in an isochronal ice-sheet model ...
topic_facet 530 Physics
description The full history of ice sheet and climate interactions is recorded in the vertical profiles of geochemical tracers in polar ice sheets. Numerical simulations of these archives promise great advances both in the interpretation of these reconstructions and the validation of the models themselves. However, fundamental mathematical shortcomings of existing models subject tracers to spurious diffusion, thwarting straightforward solutions. Here, I propose a new vertical discretization for ice-sheet models that eliminates numerical diffusion entirely. Vertical motion through the model mesh is avoided by mimicking the real-world flow of ice as a thinning of underlying layers. A new layer is added to the surface at equidistant time intervals, isochronally, thus identifying each layer uniquely by its time of deposition and age. This new approach is implemented for a two-dimensional section through the summit of the Greenland ice sheet. The ability to directly compare simulations of vertical ice cores with ...
format Text
author Born, Andreas
author_facet Born, Andreas
author_sort Born, Andreas
title Tracer transport in an isochronal ice-sheet model ...
title_short Tracer transport in an isochronal ice-sheet model ...
title_full Tracer transport in an isochronal ice-sheet model ...
title_fullStr Tracer transport in an isochronal ice-sheet model ...
title_full_unstemmed Tracer transport in an isochronal ice-sheet model ...
title_sort tracer transport in an isochronal ice-sheet model ...
publisher International Glaciological Society
publishDate 2016
url https://dx.doi.org/10.7892/boris.93879
http://boris.unibe.ch/93879/
genre Greenland
Ice Sheet
genre_facet Greenland
Ice Sheet
op_rights info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.7892/boris.93879
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