Observations of Steep Wave Statistics in Open Ocean Waters

Breaking waves are a ubiquitous phenomenon of the world's oceans. They disrupt the aqueous boundary layer causing surface renewal, thereby enhancing the diffusion of gases and heat across the air-sea interface. Breaking waves are also responsible for the dissipation of wave energy and thus dire...

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Main Authors: Scott, Nicholas V., Hara, Tetsu, Hwang, Paul A., Walsh, Edward J.
Other Authors: NAVAL RESEARCH LAB STENNIS SPACE CENTER MS OCEANOGRAPHY DIV
Format: Text
Language:English
Published: 2004
Subjects:
Online Access:http://www.dtic.mil/docs/citations/ADA442938
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA442938
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spelling ftdtic:ADA442938 2023-05-15T18:25:31+02:00 Observations of Steep Wave Statistics in Open Ocean Waters Scott, Nicholas V. Hara, Tetsu Hwang, Paul A. Walsh, Edward J. NAVAL RESEARCH LAB STENNIS SPACE CENTER MS OCEANOGRAPHY DIV 2004-08 text/html http://www.dtic.mil/docs/citations/ADA442938 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA442938 en eng http://www.dtic.mil/docs/citations/ADA442938 Approved for public release; distribution is unlimited. DTIC Physical and Dynamic Oceanography *OCEAN WAVES *OBSERVATION *STATISTICS SURFACE WAVES TOPOGRAPHY WAVE PROPAGATION BROADBAND SLOPE AMPLITUDE WAVELET TRANSFORMS STEEP WAVES SLOPE THRESHOLDS BREAKING WAVE STATISTICS WAVELET ANALYSIS BREAKING WAVES NONLINEARITY SOWEX(SOUTHERN OCEAN WAVE EXPERIMENT) PE61153N 73-8190-04-5 Text 2004 ftdtic 2016-02-22T02:34:21Z Breaking waves are a ubiquitous phenomenon of the world's oceans. They disrupt the aqueous boundary layer causing surface renewal, thereby enhancing the diffusion of gases and heat across the air-sea interface. Breaking waves are also responsible for the dissipation of wave energy and thus directly affect the evolution of the wind-wave spectrum. With advances in technology, new direct observations of the two-dimensional spatial surface wave topography have been made. These data allow for the opportunity to go beyond linear analysis and study the nonlinearity of the surface wave field, in particular the statistics of steep and breaking waves. Presented at the Conference on Interactions of the Sea and Atmosphere (13th) held in Portland, ME on 9-13 Aug 2004. Sponsored in party by the National Science Foundation Grant No. OCE0002314. Prepared in collaboration with Woods Hole Oceanographic Institution, Woods Hole, MA, Univ. of Rhode Island, Narragansett, RI and NASA/Goddard Laboratory for Hydrospheric Processes, Wallops Island, VA. Text Southern Ocean Defense Technical Information Center: DTIC Technical Reports database 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
*OCEAN WAVES
*OBSERVATION
*STATISTICS
SURFACE WAVES
TOPOGRAPHY
WAVE PROPAGATION
BROADBAND
SLOPE
AMPLITUDE
WAVELET TRANSFORMS
STEEP WAVES
SLOPE THRESHOLDS
BREAKING WAVE STATISTICS
WAVELET ANALYSIS
BREAKING WAVES
NONLINEARITY
SOWEX(SOUTHERN OCEAN WAVE EXPERIMENT)
PE61153N
73-8190-04-5
spellingShingle Physical and Dynamic Oceanography
*OCEAN WAVES
*OBSERVATION
*STATISTICS
SURFACE WAVES
TOPOGRAPHY
WAVE PROPAGATION
BROADBAND
SLOPE
AMPLITUDE
WAVELET TRANSFORMS
STEEP WAVES
SLOPE THRESHOLDS
BREAKING WAVE STATISTICS
WAVELET ANALYSIS
BREAKING WAVES
NONLINEARITY
SOWEX(SOUTHERN OCEAN WAVE EXPERIMENT)
PE61153N
73-8190-04-5
Scott, Nicholas V.
Hara, Tetsu
Hwang, Paul A.
Walsh, Edward J.
Observations of Steep Wave Statistics in Open Ocean Waters
topic_facet Physical and Dynamic Oceanography
*OCEAN WAVES
*OBSERVATION
*STATISTICS
SURFACE WAVES
TOPOGRAPHY
WAVE PROPAGATION
BROADBAND
SLOPE
AMPLITUDE
WAVELET TRANSFORMS
STEEP WAVES
SLOPE THRESHOLDS
BREAKING WAVE STATISTICS
WAVELET ANALYSIS
BREAKING WAVES
NONLINEARITY
SOWEX(SOUTHERN OCEAN WAVE EXPERIMENT)
PE61153N
73-8190-04-5
description Breaking waves are a ubiquitous phenomenon of the world's oceans. They disrupt the aqueous boundary layer causing surface renewal, thereby enhancing the diffusion of gases and heat across the air-sea interface. Breaking waves are also responsible for the dissipation of wave energy and thus directly affect the evolution of the wind-wave spectrum. With advances in technology, new direct observations of the two-dimensional spatial surface wave topography have been made. These data allow for the opportunity to go beyond linear analysis and study the nonlinearity of the surface wave field, in particular the statistics of steep and breaking waves. Presented at the Conference on Interactions of the Sea and Atmosphere (13th) held in Portland, ME on 9-13 Aug 2004. Sponsored in party by the National Science Foundation Grant No. OCE0002314. Prepared in collaboration with Woods Hole Oceanographic Institution, Woods Hole, MA, Univ. of Rhode Island, Narragansett, RI and NASA/Goddard Laboratory for Hydrospheric Processes, Wallops Island, VA.
author2 NAVAL RESEARCH LAB STENNIS SPACE CENTER MS OCEANOGRAPHY DIV
format Text
author Scott, Nicholas V.
Hara, Tetsu
Hwang, Paul A.
Walsh, Edward J.
author_facet Scott, Nicholas V.
Hara, Tetsu
Hwang, Paul A.
Walsh, Edward J.
author_sort Scott, Nicholas V.
title Observations of Steep Wave Statistics in Open Ocean Waters
title_short Observations of Steep Wave Statistics in Open Ocean Waters
title_full Observations of Steep Wave Statistics in Open Ocean Waters
title_fullStr Observations of Steep Wave Statistics in Open Ocean Waters
title_full_unstemmed Observations of Steep Wave Statistics in Open Ocean Waters
title_sort observations of steep wave statistics in open ocean waters
publishDate 2004
url http://www.dtic.mil/docs/citations/ADA442938
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA442938
geographic Southern Ocean
geographic_facet Southern Ocean
genre Southern Ocean
genre_facet Southern Ocean
op_source DTIC
op_relation http://www.dtic.mil/docs/citations/ADA442938
op_rights Approved for public release; distribution is unlimited.
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