Development of a Higher-Order Ice Sheet Model Using a Rescaled Coordinate System

The Intergovernmental Panel on Climate Change (IPCC) has estimated between 9 and 88 cm of sea level rise over the next hundred years. Of this, only negative 19 to 11 cm is attributed to the largest ice masses on the planet, the Antarctic and Greenland ice sheets. Over the last decade, dramatic activ...

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Main Authors: James Michael Fishbaugh, Dr. David, A. Strobel, Chairperson Dr. Jesse Johnson
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.569.8061
http://etd.lib.umt.edu/theses/available/etd-05302008-101724/unrestricted/fishbaughthesis.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.569.8061 2023-05-15T13:56:13+02:00 Development of a Higher-Order Ice Sheet Model Using a Rescaled Coordinate System James Michael Fishbaugh Dr. David A. Strobel Chairperson Dr. Jesse Johnson The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.569.8061 http://etd.lib.umt.edu/theses/available/etd-05302008-101724/unrestricted/fishbaughthesis.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.569.8061 http://etd.lib.umt.edu/theses/available/etd-05302008-101724/unrestricted/fishbaughthesis.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://etd.lib.umt.edu/theses/available/etd-05302008-101724/unrestricted/fishbaughthesis.pdf text ftciteseerx 2016-01-08T12:26:06Z The Intergovernmental Panel on Climate Change (IPCC) has estimated between 9 and 88 cm of sea level rise over the next hundred years. Of this, only negative 19 to 11 cm is attributed to the largest ice masses on the planet, the Antarctic and Greenland ice sheets. Over the last decade, dramatic activity in the outlet glaciers of Greenland and the Antarctic Peninsula raise the possibility that these large ice sheets will have a much greater contribution to sea level rise over the next century than was predicted by the IPCC. Recent studies have shown these areas are exhibiting decadal scale changes in response to climate forcings, whereas IPCC models show that ice is not responsive to climate change over such short periods of time. Many believe the IPCC type models fail to show short term climate responses due to the simplifications they make to ice sheet mechanics. Here, we develop a higher-order model – a new ice sheet model which contains all relevant flow physics. In order to gauge our progress, we perform a verification of our model around a structured set of experiments. The analysis reveals our model is performing well over a range of different scenarios. ii ACKNOWLEDGMENTS I would like to take this opportunity to thank all of the people who have been influential in my development as a scientist and a person during my time at the University of Montana. First, I’d like to thank Dr. Jesse Johnson for his unwavering support and for his countless explanations. Furthermore, he always treated me as a peer even when it was clear I was not. To Dr. Joel Henry, who has served as my mentor for the last several years. All my major life decisions have been influenced by his recommendations. Finally, to my peers, for all the collaboration and laughs we have shared. iii Text Antarc* Antarctic Antarctic Peninsula Greenland Ice Sheet Unknown Antarctic Antarctic Peninsula Greenland The Antarctic
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description The Intergovernmental Panel on Climate Change (IPCC) has estimated between 9 and 88 cm of sea level rise over the next hundred years. Of this, only negative 19 to 11 cm is attributed to the largest ice masses on the planet, the Antarctic and Greenland ice sheets. Over the last decade, dramatic activity in the outlet glaciers of Greenland and the Antarctic Peninsula raise the possibility that these large ice sheets will have a much greater contribution to sea level rise over the next century than was predicted by the IPCC. Recent studies have shown these areas are exhibiting decadal scale changes in response to climate forcings, whereas IPCC models show that ice is not responsive to climate change over such short periods of time. Many believe the IPCC type models fail to show short term climate responses due to the simplifications they make to ice sheet mechanics. Here, we develop a higher-order model – a new ice sheet model which contains all relevant flow physics. In order to gauge our progress, we perform a verification of our model around a structured set of experiments. The analysis reveals our model is performing well over a range of different scenarios. ii ACKNOWLEDGMENTS I would like to take this opportunity to thank all of the people who have been influential in my development as a scientist and a person during my time at the University of Montana. First, I’d like to thank Dr. Jesse Johnson for his unwavering support and for his countless explanations. Furthermore, he always treated me as a peer even when it was clear I was not. To Dr. Joel Henry, who has served as my mentor for the last several years. All my major life decisions have been influenced by his recommendations. Finally, to my peers, for all the collaboration and laughs we have shared. iii
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author James Michael Fishbaugh
Dr. David
A. Strobel
Chairperson Dr. Jesse Johnson
spellingShingle James Michael Fishbaugh
Dr. David
A. Strobel
Chairperson Dr. Jesse Johnson
Development of a Higher-Order Ice Sheet Model Using a Rescaled Coordinate System
author_facet James Michael Fishbaugh
Dr. David
A. Strobel
Chairperson Dr. Jesse Johnson
author_sort James Michael Fishbaugh
title Development of a Higher-Order Ice Sheet Model Using a Rescaled Coordinate System
title_short Development of a Higher-Order Ice Sheet Model Using a Rescaled Coordinate System
title_full Development of a Higher-Order Ice Sheet Model Using a Rescaled Coordinate System
title_fullStr Development of a Higher-Order Ice Sheet Model Using a Rescaled Coordinate System
title_full_unstemmed Development of a Higher-Order Ice Sheet Model Using a Rescaled Coordinate System
title_sort development of a higher-order ice sheet model using a rescaled coordinate system
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.569.8061
http://etd.lib.umt.edu/theses/available/etd-05302008-101724/unrestricted/fishbaughthesis.pdf
geographic Antarctic
Antarctic Peninsula
Greenland
The Antarctic
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Antarctic Peninsula
Greenland
The Antarctic
genre Antarc*
Antarctic
Antarctic Peninsula
Greenland
Ice Sheet
genre_facet Antarc*
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Antarctic Peninsula
Greenland
Ice Sheet
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http://etd.lib.umt.edu/theses/available/etd-05302008-101724/unrestricted/fishbaughthesis.pdf
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