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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Bibliographic Details
Main Author: Cooper, Vincent T.
Other Authors: Bitz, Cecilia
Format: Thesis
Language:English
Published: 2022
Subjects:
Online Access:http://hdl.handle.net/1773/48437
id ftunivwashington:oai:digital.lib.washington.edu:1773/48437
record_format openpolar
spelling 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
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