Modelling long term ice sheet changes to understand the stability of the Greenland Ice Sheet in a warmer world

The Greenland Ice Sheet is under stress with the rising temperature. Ice sheet sensitivity to temperature changes and its contribution to global sea level rise can be estimated using ice sheet/climate models. This study combines an ice dynamics model and an isotope tracer model to carry out long-ter...

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Bibliographic Details
Main Author: Rahimian, Zahra
Other Authors: Marshall, Shawn, Else, Brent G. T., Norman, Ann-Lise
Format: Master Thesis
Language:English
Published: Arts 2020
Subjects:
Online Access:http://hdl.handle.net/1880/111561
https://doi.org/10.11575/PRISM/37509
id ftunivcalgary:oai:prism.ucalgary.ca:1880/111561
record_format openpolar
spelling ftunivcalgary:oai:prism.ucalgary.ca:1880/111561 2023-08-27T04:09:40+02:00 Modelling long term ice sheet changes to understand the stability of the Greenland Ice Sheet in a warmer world Rahimian, Zahra Marshall, Shawn Else, Brent G. T. Norman, Ann-Lise 2020-01-24 application/pdf http://hdl.handle.net/1880/111561 https://doi.org/10.11575/PRISM/37509 eng eng Arts University of Calgary Rahimian, Z. (2020). Modelling long term ice sheet changes to understand the stability of the Greenland Ice Sheet in a warmer world (Unpublished master's thesis). University of Calgary, Calgary, AB. http://dx.doi.org/10.11575/PRISM/37509 http://hdl.handle.net/1880/111561 University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission. Physical Geography Environmental Sciences master thesis 2020 ftunivcalgary https://doi.org/10.11575/PRISM/37509 2023-08-06T06:36:46Z The Greenland Ice Sheet is under stress with the rising temperature. Ice sheet sensitivity to temperature changes and its contribution to global sea level rise can be estimated using ice sheet/climate models. This study combines an ice dynamics model and an isotope tracer model to carry out long-term coupled ice-sheet/climate simulations to investigate the vulnerability of the Greenland ice sheet to higher temperatures during the Eemian warming. I also examine how Eemian melting may have altered isotopic ratios and temperature reconstructions. The simulations are benchmarked against NEEM and Summit ice core observations to provide validation of model performance. I find that there is ice in central Greenland for climates up to 12ºC higher than present. Greenland’s contribution due to Eemian sea level most likely ranges between 2.8 to 4.3 m, associated with temperature anomalies from 5 to 9ºC. Melt-induced isotopic modifications can cause overestimation of 0.1-2ºC warming in proxy records. Master Thesis Greenland ice core Ice Sheet PRISM - University of Calgary Digital Repository Greenland
institution Open Polar
collection PRISM - University of Calgary Digital Repository
op_collection_id ftunivcalgary
language English
topic Physical Geography
Environmental Sciences
spellingShingle Physical Geography
Environmental Sciences
Rahimian, Zahra
Modelling long term ice sheet changes to understand the stability of the Greenland Ice Sheet in a warmer world
topic_facet Physical Geography
Environmental Sciences
description The Greenland Ice Sheet is under stress with the rising temperature. Ice sheet sensitivity to temperature changes and its contribution to global sea level rise can be estimated using ice sheet/climate models. This study combines an ice dynamics model and an isotope tracer model to carry out long-term coupled ice-sheet/climate simulations to investigate the vulnerability of the Greenland ice sheet to higher temperatures during the Eemian warming. I also examine how Eemian melting may have altered isotopic ratios and temperature reconstructions. The simulations are benchmarked against NEEM and Summit ice core observations to provide validation of model performance. I find that there is ice in central Greenland for climates up to 12ºC higher than present. Greenland’s contribution due to Eemian sea level most likely ranges between 2.8 to 4.3 m, associated with temperature anomalies from 5 to 9ºC. Melt-induced isotopic modifications can cause overestimation of 0.1-2ºC warming in proxy records.
author2 Marshall, Shawn
Else, Brent G. T.
Norman, Ann-Lise
format Master Thesis
author Rahimian, Zahra
author_facet Rahimian, Zahra
author_sort Rahimian, Zahra
title Modelling long term ice sheet changes to understand the stability of the Greenland Ice Sheet in a warmer world
title_short Modelling long term ice sheet changes to understand the stability of the Greenland Ice Sheet in a warmer world
title_full Modelling long term ice sheet changes to understand the stability of the Greenland Ice Sheet in a warmer world
title_fullStr Modelling long term ice sheet changes to understand the stability of the Greenland Ice Sheet in a warmer world
title_full_unstemmed Modelling long term ice sheet changes to understand the stability of the Greenland Ice Sheet in a warmer world
title_sort modelling long term ice sheet changes to understand the stability of the greenland ice sheet in a warmer world
publisher Arts
publishDate 2020
url http://hdl.handle.net/1880/111561
https://doi.org/10.11575/PRISM/37509
geographic Greenland
geographic_facet Greenland
genre Greenland
ice core
Ice Sheet
genre_facet Greenland
ice core
Ice Sheet
op_relation Rahimian, Z. (2020). Modelling long term ice sheet changes to understand the stability of the Greenland Ice Sheet in a warmer world (Unpublished master's thesis). University of Calgary, Calgary, AB.
http://dx.doi.org/10.11575/PRISM/37509
http://hdl.handle.net/1880/111561
op_rights University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission.
op_doi https://doi.org/10.11575/PRISM/37509
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