Wind Waves in Sea Ice of the Western Arctic and a Global Coupled Wave-Ice Model
Thesis (Master's)--University of Washington, 2022 The retreat of Arctic sea ice is enabling increased ocean wave activity at the ice edge, yet the interactions between surface waves and sea ice are not fully understood. Here, we examine in situ observations of wave spectra spanning 2012-2021 in...
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ftunivwashington:oai:digital.lib.washington.edu:1773/48437 2023-05-15T14:53:38+02:00 Wind Waves in Sea Ice of the Western Arctic and a Global Coupled Wave-Ice Model Cooper, Vincent T. Bitz, Cecilia 2022 application/pdf http://hdl.handle.net/1773/48437 en_US eng Cooper_washington_0250O_23944.pdf http://hdl.handle.net/1773/48437 none coupled wave-ice model field observations marginal ice zone ocean waves sea ice wave attenuation Atmospheric sciences Physical oceanography Climate change Thesis 2022 ftunivwashington 2023-03-12T19:01:27Z Thesis (Master's)--University of Washington, 2022 The retreat of Arctic sea ice is enabling increased ocean wave activity at the ice edge, yet the interactions between surface waves and sea ice are not fully understood. Here, we examine in situ observations of wave spectra spanning 2012-2021 in the western Arctic marginal ice zone (MIZ). Swell waves are rarely observed beyond 100 km inside the MIZ. However, local wind waves are observed forming in patches of open water amid partial ice cover during summer. These local waves remain fetch-limited between ice floes with heights less than 1 m. To investigate the physics of these waves, we conduct experiments varying wave attenuation and generation in ice in a global model with coupled interactions between waves and sea ice. A weak high-frequency attenuation rate is required to simulate the wind waves reported in observations. The choice of attenuation scheme and the wind input in ice have a remarkable impact on the extent of wave activity in sea ice across polar oceans, particularly in the Southern Hemisphere. As well as demonstrating the need for stronger constraints on wave attenuation, our results suggest further attention should be paid to locally generated wind waves and their role in sea ice evolution. Thesis Arctic Climate change Sea ice University of Washington, Seattle: ResearchWorks Arctic |
institution |
Open Polar |
collection |
University of Washington, Seattle: ResearchWorks |
op_collection_id |
ftunivwashington |
language |
English |
topic |
coupled wave-ice model field observations marginal ice zone ocean waves sea ice wave attenuation Atmospheric sciences Physical oceanography Climate change |
spellingShingle |
coupled wave-ice model field observations marginal ice zone ocean waves sea ice wave attenuation Atmospheric sciences Physical oceanography Climate change Cooper, Vincent T. Wind Waves in Sea Ice of the Western Arctic and a Global Coupled Wave-Ice Model |
topic_facet |
coupled wave-ice model field observations marginal ice zone ocean waves sea ice wave attenuation Atmospheric sciences Physical oceanography Climate change |
description |
Thesis (Master's)--University of Washington, 2022 The retreat of Arctic sea ice is enabling increased ocean wave activity at the ice edge, yet the interactions between surface waves and sea ice are not fully understood. Here, we examine in situ observations of wave spectra spanning 2012-2021 in the western Arctic marginal ice zone (MIZ). Swell waves are rarely observed beyond 100 km inside the MIZ. However, local wind waves are observed forming in patches of open water amid partial ice cover during summer. These local waves remain fetch-limited between ice floes with heights less than 1 m. To investigate the physics of these waves, we conduct experiments varying wave attenuation and generation in ice in a global model with coupled interactions between waves and sea ice. A weak high-frequency attenuation rate is required to simulate the wind waves reported in observations. The choice of attenuation scheme and the wind input in ice have a remarkable impact on the extent of wave activity in sea ice across polar oceans, particularly in the Southern Hemisphere. As well as demonstrating the need for stronger constraints on wave attenuation, our results suggest further attention should be paid to locally generated wind waves and their role in sea ice evolution. |
author2 |
Bitz, Cecilia |
format |
Thesis |
author |
Cooper, Vincent T. |
author_facet |
Cooper, Vincent T. |
author_sort |
Cooper, Vincent T. |
title |
Wind Waves in Sea Ice of the Western Arctic and a Global Coupled Wave-Ice Model |
title_short |
Wind Waves in Sea Ice of the Western Arctic and a Global Coupled Wave-Ice Model |
title_full |
Wind Waves in Sea Ice of the Western Arctic and a Global Coupled Wave-Ice Model |
title_fullStr |
Wind Waves in Sea Ice of the Western Arctic and a Global Coupled Wave-Ice Model |
title_full_unstemmed |
Wind Waves in Sea Ice of the Western Arctic and a Global Coupled Wave-Ice Model |
title_sort |
wind waves in sea ice of the western arctic and a global coupled wave-ice model |
publishDate |
2022 |
url |
http://hdl.handle.net/1773/48437 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Climate change Sea ice |
genre_facet |
Arctic Climate change Sea ice |
op_relation |
Cooper_washington_0250O_23944.pdf http://hdl.handle.net/1773/48437 |
op_rights |
none |
_version_ |
1766325233758765056 |