Simple models for the simulation of submarine melt for a Greenland glacial system model
Two hundred marine-terminating Greenland outlet glaciers deliver more than half of the annually accumulated ice into the ocean and have played an important role in the Greenland ice sheet mass loss observed since the mid-1990s. Submarine melt may play a crucial role in the mass balance and position...
Main Authors: | , , |
---|---|
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
München : European Geopyhsical Union
2018
|
Subjects: | |
Online Access: | https://oa.tib.eu/renate/handle/123456789/667 https://doi.org/10.34657/1255 |
id |
fttibhannoverren:oai:oa.tib.eu:123456789/667 |
---|---|
record_format |
openpolar |
spelling |
fttibhannoverren:oai:oa.tib.eu:123456789/667 2023-05-15T16:21:12+02:00 Simple models for the simulation of submarine melt for a Greenland glacial system model Beckmann, Johanna Perrette, Mahé Ganopolski, Andrey 2018 application/pdf https://oa.tib.eu/renate/handle/123456789/667 https://doi.org/10.34657/1255 eng eng München : European Geopyhsical Union DOI:https://doi.org/10.5194/tc-12-301-2018 https://doi.org/10.34657/1255 https://oa.tib.eu/renate/handle/123456789/667 CC BY 3.0 Unported https://creativecommons.org/licenses/by/3.0/ frei zugänglich CC-BY The Cryosphere, Volume 12, Issue 1, Page 301-323 General circulation model glacier glacier mass balance glacier retreat grounding line ice core ice sheet numerical model plume sea level change simulation underwater environment ddc:550 status-type:publishedVersion doc-type:article doc-type:Text 2018 fttibhannoverren https://doi.org/10.34657/1255 https://doi.org/10.5194/tc-12-301-2018 2022-09-19T16:17:59Z Two hundred marine-terminating Greenland outlet glaciers deliver more than half of the annually accumulated ice into the ocean and have played an important role in the Greenland ice sheet mass loss observed since the mid-1990s. Submarine melt may play a crucial role in the mass balance and position of the grounding line of these outlet glaciers. As the ocean warms, it is expected that submarine melt will increase, potentially driving outlet glaciers retreat and contributing to sea level rise. Projections of the future contribution of outlet glaciers to sea level rise are hampered by the necessity to use models with extremely high resolution of the order of a few hundred meters. That requirement in not only demanded when modeling outlet glaciers as a stand alone model but also when coupling them with high-resolution 3-D ocean models. In addition, fjord bathymetry data are mostly missing or inaccurate (errors of several hundreds of meters), which questions the benefit of using computationally expensive 3-D models for future predictions. Here we propose an alternative approach built on the use of a computationally efficient simple model of submarine melt based on turbulent plume theory. We show that such a simple model is in reasonable agreement with several available modeling studies. We performed a suite of experiments to analyze sensitivity of these simple models to model parameters and climate characteristics. We found that the computationally cheap plume model demonstrates qualitatively similar behavior as 3-D general circulation models. To match results of the 3-D models in a quantitative manner, a scaling factor of the order of 1 is needed for the plume models. We applied this approach to model submarine melt for six representative Greenland glaciers and found that the application of a line plume can produce submarine melt compatible with observational data. Our results show that the line plume model is more appropriate than the cone plume model for simulating the average submarine melting of real glaciers ... Article in Journal/Newspaper glacier Greenland ice core Ice Sheet The Cryosphere Renate - Repositorium für Naturwissenschaften und Technik (TIB Hannover) Greenland |
institution |
Open Polar |
collection |
Renate - Repositorium für Naturwissenschaften und Technik (TIB Hannover) |
op_collection_id |
fttibhannoverren |
language |
English |
topic |
General circulation model glacier glacier mass balance glacier retreat grounding line ice core ice sheet numerical model plume sea level change simulation underwater environment ddc:550 |
spellingShingle |
General circulation model glacier glacier mass balance glacier retreat grounding line ice core ice sheet numerical model plume sea level change simulation underwater environment ddc:550 Beckmann, Johanna Perrette, Mahé Ganopolski, Andrey Simple models for the simulation of submarine melt for a Greenland glacial system model |
topic_facet |
General circulation model glacier glacier mass balance glacier retreat grounding line ice core ice sheet numerical model plume sea level change simulation underwater environment ddc:550 |
description |
Two hundred marine-terminating Greenland outlet glaciers deliver more than half of the annually accumulated ice into the ocean and have played an important role in the Greenland ice sheet mass loss observed since the mid-1990s. Submarine melt may play a crucial role in the mass balance and position of the grounding line of these outlet glaciers. As the ocean warms, it is expected that submarine melt will increase, potentially driving outlet glaciers retreat and contributing to sea level rise. Projections of the future contribution of outlet glaciers to sea level rise are hampered by the necessity to use models with extremely high resolution of the order of a few hundred meters. That requirement in not only demanded when modeling outlet glaciers as a stand alone model but also when coupling them with high-resolution 3-D ocean models. In addition, fjord bathymetry data are mostly missing or inaccurate (errors of several hundreds of meters), which questions the benefit of using computationally expensive 3-D models for future predictions. Here we propose an alternative approach built on the use of a computationally efficient simple model of submarine melt based on turbulent plume theory. We show that such a simple model is in reasonable agreement with several available modeling studies. We performed a suite of experiments to analyze sensitivity of these simple models to model parameters and climate characteristics. We found that the computationally cheap plume model demonstrates qualitatively similar behavior as 3-D general circulation models. To match results of the 3-D models in a quantitative manner, a scaling factor of the order of 1 is needed for the plume models. We applied this approach to model submarine melt for six representative Greenland glaciers and found that the application of a line plume can produce submarine melt compatible with observational data. Our results show that the line plume model is more appropriate than the cone plume model for simulating the average submarine melting of real glaciers ... |
format |
Article in Journal/Newspaper |
author |
Beckmann, Johanna Perrette, Mahé Ganopolski, Andrey |
author_facet |
Beckmann, Johanna Perrette, Mahé Ganopolski, Andrey |
author_sort |
Beckmann, Johanna |
title |
Simple models for the simulation of submarine melt for a Greenland glacial system model |
title_short |
Simple models for the simulation of submarine melt for a Greenland glacial system model |
title_full |
Simple models for the simulation of submarine melt for a Greenland glacial system model |
title_fullStr |
Simple models for the simulation of submarine melt for a Greenland glacial system model |
title_full_unstemmed |
Simple models for the simulation of submarine melt for a Greenland glacial system model |
title_sort |
simple models for the simulation of submarine melt for a greenland glacial system model |
publisher |
München : European Geopyhsical Union |
publishDate |
2018 |
url |
https://oa.tib.eu/renate/handle/123456789/667 https://doi.org/10.34657/1255 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
glacier Greenland ice core Ice Sheet The Cryosphere |
genre_facet |
glacier Greenland ice core Ice Sheet The Cryosphere |
op_source |
The Cryosphere, Volume 12, Issue 1, Page 301-323 |
op_relation |
DOI:https://doi.org/10.5194/tc-12-301-2018 https://doi.org/10.34657/1255 https://oa.tib.eu/renate/handle/123456789/667 |
op_rights |
CC BY 3.0 Unported https://creativecommons.org/licenses/by/3.0/ frei zugänglich |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.34657/1255 https://doi.org/10.5194/tc-12-301-2018 |
_version_ |
1766009210773962752 |