High-Resolution Regional Wave Hindcast for the U.S. Alaska Coast

Regional long-term wave hindcast with state-of-art third-generation models is essential for characterization of regional wave resources. This report summarizes modeling efforts for the simulation of the wave climate along southern Alaska, which used an unstructured, nested-grid modeling approach tha...

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Main Authors: Yang, Zhaoqing, Wu, Wei-Cheng, Wang, Taiping, Garcia Medina, Gabriel, Castrucci, Luca
Language:unknown
Published: 2021
Subjects:
Online Access:http://www.osti.gov/servlets/purl/1579259
https://www.osti.gov/biblio/1579259
https://doi.org/10.2172/1579259
id ftosti:oai:osti.gov:1579259
record_format openpolar
spelling ftosti:oai:osti.gov:1579259 2023-07-30T04:02:41+02:00 High-Resolution Regional Wave Hindcast for the U.S. Alaska Coast Yang, Zhaoqing Wu, Wei-Cheng Wang, Taiping Garcia Medina, Gabriel Castrucci, Luca 2021-03-31 application/pdf http://www.osti.gov/servlets/purl/1579259 https://www.osti.gov/biblio/1579259 https://doi.org/10.2172/1579259 unknown http://www.osti.gov/servlets/purl/1579259 https://www.osti.gov/biblio/1579259 https://doi.org/10.2172/1579259 doi:10.2172/1579259 2021 ftosti https://doi.org/10.2172/1579259 2023-07-11T09:38:27Z Regional long-term wave hindcast with state-of-art third-generation models is essential for characterization of regional wave resources. This report summarizes modeling efforts for the simulation of the wave climate along southern Alaska, which used an unstructured, nested-grid modeling approach that incorporates a global-regional nested grid using WAVEWATCH III ® and the high-resolution SWAN (Simulating Waves Nearshore) model. Wave resource and wave bulk parameters were simulated for a 32-year period from 1979 to 2010 and were subsequently validated with wave buoy data in the model domain. Error statistics of model skills were calculated at all buoy stations. Overall, model results, both resource and bulk parameters, match observations well. The model hindcast was able to reproduce the seasonal variation of the sea state with large waves that occur in the winter and early spring months when wind forcing is strong and the calm sea state during the summer when wind forcing is weak. The hindcast also considers the effect of sea ice on wave growth, which affects the southern Bering Sea. The hindcast results, including resource and bulk parameters, were archived at every model grid point for the entire model domain at three-hour intervals. In addition, spectral results were saved at National Data Buoy Center buoy stations and selected virtual buoy locations at hourly intervals. The nested-grid modeling framework employed in this study provides a powerful and efficient modeling approach for accurately simulating wave climate at regional and long-term temporal scales with sufficiently fine resolutions in the nearshore region. Other/Unknown Material Bering Sea Sea ice Alaska SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy) Bering Sea
institution Open Polar
collection SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy)
op_collection_id ftosti
language unknown
description Regional long-term wave hindcast with state-of-art third-generation models is essential for characterization of regional wave resources. This report summarizes modeling efforts for the simulation of the wave climate along southern Alaska, which used an unstructured, nested-grid modeling approach that incorporates a global-regional nested grid using WAVEWATCH III ® and the high-resolution SWAN (Simulating Waves Nearshore) model. Wave resource and wave bulk parameters were simulated for a 32-year period from 1979 to 2010 and were subsequently validated with wave buoy data in the model domain. Error statistics of model skills were calculated at all buoy stations. Overall, model results, both resource and bulk parameters, match observations well. The model hindcast was able to reproduce the seasonal variation of the sea state with large waves that occur in the winter and early spring months when wind forcing is strong and the calm sea state during the summer when wind forcing is weak. The hindcast also considers the effect of sea ice on wave growth, which affects the southern Bering Sea. The hindcast results, including resource and bulk parameters, were archived at every model grid point for the entire model domain at three-hour intervals. In addition, spectral results were saved at National Data Buoy Center buoy stations and selected virtual buoy locations at hourly intervals. The nested-grid modeling framework employed in this study provides a powerful and efficient modeling approach for accurately simulating wave climate at regional and long-term temporal scales with sufficiently fine resolutions in the nearshore region.
author Yang, Zhaoqing
Wu, Wei-Cheng
Wang, Taiping
Garcia Medina, Gabriel
Castrucci, Luca
spellingShingle Yang, Zhaoqing
Wu, Wei-Cheng
Wang, Taiping
Garcia Medina, Gabriel
Castrucci, Luca
High-Resolution Regional Wave Hindcast for the U.S. Alaska Coast
author_facet Yang, Zhaoqing
Wu, Wei-Cheng
Wang, Taiping
Garcia Medina, Gabriel
Castrucci, Luca
author_sort Yang, Zhaoqing
title High-Resolution Regional Wave Hindcast for the U.S. Alaska Coast
title_short High-Resolution Regional Wave Hindcast for the U.S. Alaska Coast
title_full High-Resolution Regional Wave Hindcast for the U.S. Alaska Coast
title_fullStr High-Resolution Regional Wave Hindcast for the U.S. Alaska Coast
title_full_unstemmed High-Resolution Regional Wave Hindcast for the U.S. Alaska Coast
title_sort high-resolution regional wave hindcast for the u.s. alaska coast
publishDate 2021
url http://www.osti.gov/servlets/purl/1579259
https://www.osti.gov/biblio/1579259
https://doi.org/10.2172/1579259
geographic Bering Sea
geographic_facet Bering Sea
genre Bering Sea
Sea ice
Alaska
genre_facet Bering Sea
Sea ice
Alaska
op_relation http://www.osti.gov/servlets/purl/1579259
https://www.osti.gov/biblio/1579259
https://doi.org/10.2172/1579259
doi:10.2172/1579259
op_doi https://doi.org/10.2172/1579259
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