Hindcasting Swell from the Southern Ocean Along the U.S. Pacific Coast.
It is well documented that ocean swell arrives at the U.S. Pacific coast especially southern California, from the Southern Ocean during the Northern Hemisphere summer. This swell can have a major impact on sand transport in the littoral zone as it shoals and breaks on the beach. Hindcast wave inform...
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ftdtic:ADA294220 2023-05-15T18:24:45+02:00 Hindcasting Swell from the Southern Ocean Along the U.S. Pacific Coast. Hubertz, J. M. Payne, J. B. Farrar, P. D. ARMY ENGINEER WATERWAYS EXPERIMENT STATION VICKSBURG MS 1995-03 text/html http://www.dtic.mil/docs/citations/ADA294220 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA294220 en eng http://www.dtic.mil/docs/citations/ADA294220 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Physical and Dynamic Oceanography *FORECASTING *SEA STATES WIND SEASONAL VARIATIONS CALIFORNIA PACIFIC OCEAN HINDCASTING WISWAVE 2.0 COMPUTER PROGRAM Text 1995 ftdtic 2016-02-19T12:27:30Z It is well documented that ocean swell arrives at the U.S. Pacific coast especially southern California, from the Southern Ocean during the Northern Hemisphere summer. This swell can have a major impact on sand transport in the littoral zone as it shoals and breaks on the beach. Hindcast wave information for this region does not contain this component of the wave climate. This report describes a method by which this swell can be included in future wave hindcasts. Buoy wave measurements are analyzed to identify and characterize swell from the Southern Hemisphere. The Wave Information Study wave model WISWAVE 2.0 is used to hindcast swell from a hypothetical storm in the Southern Hemisphere as well as actual storms during the summers of 1988 and 1989. Hindcast results are compared to theory and measurements. Swell heights calculated by the model tend to be higher than those determined from measurements. Differences are attributed to loss of swell energy during propagation through the south Pacific islands not represented in the model and possibly to inaccurate wind speeds and directions over the Southern Ocean. Despite differences, the approach is considered practical if model results are calibrated to measurements. Text Southern Ocean Defense Technical Information Center: DTIC Technical Reports database Pacific Southern Ocean |
institution |
Open Polar |
collection |
Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
Physical and Dynamic Oceanography *FORECASTING *SEA STATES WIND SEASONAL VARIATIONS CALIFORNIA PACIFIC OCEAN HINDCASTING WISWAVE 2.0 COMPUTER PROGRAM |
spellingShingle |
Physical and Dynamic Oceanography *FORECASTING *SEA STATES WIND SEASONAL VARIATIONS CALIFORNIA PACIFIC OCEAN HINDCASTING WISWAVE 2.0 COMPUTER PROGRAM Hubertz, J. M. Payne, J. B. Farrar, P. D. Hindcasting Swell from the Southern Ocean Along the U.S. Pacific Coast. |
topic_facet |
Physical and Dynamic Oceanography *FORECASTING *SEA STATES WIND SEASONAL VARIATIONS CALIFORNIA PACIFIC OCEAN HINDCASTING WISWAVE 2.0 COMPUTER PROGRAM |
description |
It is well documented that ocean swell arrives at the U.S. Pacific coast especially southern California, from the Southern Ocean during the Northern Hemisphere summer. This swell can have a major impact on sand transport in the littoral zone as it shoals and breaks on the beach. Hindcast wave information for this region does not contain this component of the wave climate. This report describes a method by which this swell can be included in future wave hindcasts. Buoy wave measurements are analyzed to identify and characterize swell from the Southern Hemisphere. The Wave Information Study wave model WISWAVE 2.0 is used to hindcast swell from a hypothetical storm in the Southern Hemisphere as well as actual storms during the summers of 1988 and 1989. Hindcast results are compared to theory and measurements. Swell heights calculated by the model tend to be higher than those determined from measurements. Differences are attributed to loss of swell energy during propagation through the south Pacific islands not represented in the model and possibly to inaccurate wind speeds and directions over the Southern Ocean. Despite differences, the approach is considered practical if model results are calibrated to measurements. |
author2 |
ARMY ENGINEER WATERWAYS EXPERIMENT STATION VICKSBURG MS |
format |
Text |
author |
Hubertz, J. M. Payne, J. B. Farrar, P. D. |
author_facet |
Hubertz, J. M. Payne, J. B. Farrar, P. D. |
author_sort |
Hubertz, J. M. |
title |
Hindcasting Swell from the Southern Ocean Along the U.S. Pacific Coast. |
title_short |
Hindcasting Swell from the Southern Ocean Along the U.S. Pacific Coast. |
title_full |
Hindcasting Swell from the Southern Ocean Along the U.S. Pacific Coast. |
title_fullStr |
Hindcasting Swell from the Southern Ocean Along the U.S. Pacific Coast. |
title_full_unstemmed |
Hindcasting Swell from the Southern Ocean Along the U.S. Pacific Coast. |
title_sort |
hindcasting swell from the southern ocean along the u.s. pacific coast. |
publishDate |
1995 |
url |
http://www.dtic.mil/docs/citations/ADA294220 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA294220 |
geographic |
Pacific Southern Ocean |
geographic_facet |
Pacific Southern Ocean |
genre |
Southern Ocean |
genre_facet |
Southern Ocean |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/ADA294220 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
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1766205612891308032 |