Wave heights in the 21st century Arctic Ocean simulated with a regional climate model

While wave heights globally have been growing over recent decades, observations of their regional trends vary. Simulations of future wave climate can be achieved by coupling wave and climate models. At present, wave heights and their future trends in the Arctic Ocean remain unknown. We use the third...

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Published in:Geophysical Research Letters
Main Authors: Khon, V. C., Mokhov, I. I., Pogarskiy, F. A., Babanin, A., Dethloff, K., Rinke, A., Matthes, H.
Other Authors: Swinburne University of Technology
Format: Article in Journal/Newspaper
Language:unknown
Published: Wiley 2014
Subjects:
Online Access:http://hdl.handle.net/1959.3/381831
https://doi.org/10.1002/2014GL059847
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spelling ftswinburne:tle:3f4e4ccc-bff6-4342-8c15-4892551cc03b:28f49f06-0da8-44be-9edc-ad1dd0a9c582:1 2023-05-15T14:37:43+02:00 Wave heights in the 21st century Arctic Ocean simulated with a regional climate model Khon, V. C. Mokhov, I. I. Pogarskiy, F. A. Babanin, A. Dethloff, K. Rinke, A. Matthes, H. Swinburne University of Technology 2014 http://hdl.handle.net/1959.3/381831 https://doi.org/10.1002/2014GL059847 unknown Wiley http://hdl.handle.net/1959.3/381831 https://doi.org/10.1002/2014GL059847 Copyright © 2014 American Geophysical Union. The published version is reproduced in accordance with the copyright policy of the publisher. Geophysical Research Letters, Vol. 41, no. 8 (Apr 2014), pp. 2956-2961 Journal article 2014 ftswinburne https://doi.org/10.1002/2014GL059847 2019-09-07T20:58:44Z While wave heights globally have been growing over recent decades, observations of their regional trends vary. Simulations of future wave climate can be achieved by coupling wave and climate models. At present, wave heights and their future trends in the Arctic Ocean remain unknown. We use the third-generation wave forecast model WAVEWATCH-III forced by winds and sea ice concentration produced within the regional model HIRHAM, under the anthropogenic scenario SRES-A1B. We find that significant wave height and its extremes will increase over different inner Arctic areas due to reduction of sea ice cover and regional wind intensification in the 21st century. The opposite tendency, with a slight reduction in wave height appears for the Atlantic sector and the Barents Sea. Our results demonstrate the complex wave response in the Arctic Ocean to a combined effect of wind and sea ice forcings in a climate-change scenario during the 21st century. Key Points Significant wave height will increase over the Arctic Ocean in the 21st century Reduction in wave height is expected for the Atlantic sector and the Barents Sea. Article in Journal/Newspaper Arctic Arctic Ocean Barents Sea Climate change Sea ice Swinburne University of Technology: Swinburne Research Bank Arctic Arctic Ocean Barents Sea Geophysical Research Letters 41 8 2956 2961
institution Open Polar
collection Swinburne University of Technology: Swinburne Research Bank
op_collection_id ftswinburne
language unknown
description While wave heights globally have been growing over recent decades, observations of their regional trends vary. Simulations of future wave climate can be achieved by coupling wave and climate models. At present, wave heights and their future trends in the Arctic Ocean remain unknown. We use the third-generation wave forecast model WAVEWATCH-III forced by winds and sea ice concentration produced within the regional model HIRHAM, under the anthropogenic scenario SRES-A1B. We find that significant wave height and its extremes will increase over different inner Arctic areas due to reduction of sea ice cover and regional wind intensification in the 21st century. The opposite tendency, with a slight reduction in wave height appears for the Atlantic sector and the Barents Sea. Our results demonstrate the complex wave response in the Arctic Ocean to a combined effect of wind and sea ice forcings in a climate-change scenario during the 21st century. Key Points Significant wave height will increase over the Arctic Ocean in the 21st century Reduction in wave height is expected for the Atlantic sector and the Barents Sea.
author2 Swinburne University of Technology
format Article in Journal/Newspaper
author Khon, V. C.
Mokhov, I. I.
Pogarskiy, F. A.
Babanin, A.
Dethloff, K.
Rinke, A.
Matthes, H.
spellingShingle Khon, V. C.
Mokhov, I. I.
Pogarskiy, F. A.
Babanin, A.
Dethloff, K.
Rinke, A.
Matthes, H.
Wave heights in the 21st century Arctic Ocean simulated with a regional climate model
author_facet Khon, V. C.
Mokhov, I. I.
Pogarskiy, F. A.
Babanin, A.
Dethloff, K.
Rinke, A.
Matthes, H.
author_sort Khon, V. C.
title Wave heights in the 21st century Arctic Ocean simulated with a regional climate model
title_short Wave heights in the 21st century Arctic Ocean simulated with a regional climate model
title_full Wave heights in the 21st century Arctic Ocean simulated with a regional climate model
title_fullStr Wave heights in the 21st century Arctic Ocean simulated with a regional climate model
title_full_unstemmed Wave heights in the 21st century Arctic Ocean simulated with a regional climate model
title_sort wave heights in the 21st century arctic ocean simulated with a regional climate model
publisher Wiley
publishDate 2014
url http://hdl.handle.net/1959.3/381831
https://doi.org/10.1002/2014GL059847
geographic Arctic
Arctic Ocean
Barents Sea
geographic_facet Arctic
Arctic Ocean
Barents Sea
genre Arctic
Arctic Ocean
Barents Sea
Climate change
Sea ice
genre_facet Arctic
Arctic Ocean
Barents Sea
Climate change
Sea ice
op_source Geophysical Research Letters, Vol. 41, no. 8 (Apr 2014), pp. 2956-2961
op_relation http://hdl.handle.net/1959.3/381831
https://doi.org/10.1002/2014GL059847
op_rights Copyright © 2014 American Geophysical Union. The published version is reproduced in accordance with the copyright policy of the publisher.
op_doi https://doi.org/10.1002/2014GL059847
container_title Geophysical Research Letters
container_volume 41
container_issue 8
container_start_page 2956
op_container_end_page 2961
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