Secretary of the Navy Professor of Oceanography

The principal research effort has been towards understanding the high-frequency tail of the surface gravity wave spectrum, lengths of 2 cm to 60 cm; these a principally responsible for wind drag on water. Analysis was based on a unique data set from geophones and hydrophones at 5 1/2 km depth midway...

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Main Author: Munk, Walter
Other Authors: SCRIPPS INSTITUTION OF OCEANOGRAPHY LA JOLLA CA
Format: Text
Language:English
Published: 2011
Subjects:
ICE
Online Access:http://www.dtic.mil/docs/citations/ADA542691
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA542691
id ftdtic:ADA542691
record_format openpolar
spelling ftdtic:ADA542691 2023-05-15T14:57:07+02:00 Secretary of the Navy Professor of Oceanography Munk, Walter SCRIPPS INSTITUTION OF OCEANOGRAPHY LA JOLLA CA 2011-02-28 text/html http://www.dtic.mil/docs/citations/ADA542691 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA542691 en eng http://www.dtic.mil/docs/citations/ADA542691 Approved for public release; distribution is unlimited. DTIC Physical and Dynamic Oceanography *OCEAN SURFACE *GRAVITY WAVES WIND BIBLIOGRAPHIES SPECTRA ACOUSTIC TOMOGRAPHY MELTING TOMOGRAPHY SEA LEVEL ROSS SEA ARCTIC OCEAN MONITORING POLAR REGIONS ICE ARCTIC OCEANOGRAPHY CAPILLARIES OCEAN SURFACE ROUGHNESS POLAR ICE SEA LEVEL RISE WIND DRAG Text 2011 ftdtic 2016-02-23T07:48:09Z The principal research effort has been towards understanding the high-frequency tail of the surface gravity wave spectrum, lengths of 2 cm to 60 cm; these a principally responsible for wind drag on water. Analysis was based on a unique data set from geophones and hydrophones at 5 1/2 km depth midway between California and Hawaii. The measured spectral intensity around 10 Hz gives a more accurate measure of local winds than the standard satellite scatterometry. A spectral gap at the 30 Hz gravity to capillary transition offers new opportunities for spectral monitoring. We are making progress towards understanding the generation processes A continuing effort towards the acoustic monitoring of ocean processes has been directed at the polar ocean cavities sandwiched between the floating ice sheet and the sea floor. We are exploring a possible tomography experiment in the Ross Sea with the goal of better predicting polar ice melting processes and the associated global rise in sea level. Text Arctic Arctic Ocean Ice Sheet Ross Sea Defense Technical Information Center: DTIC Technical Reports database Arctic Arctic Ocean Ross Sea
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Physical and Dynamic Oceanography
*OCEAN SURFACE
*GRAVITY WAVES
WIND
BIBLIOGRAPHIES
SPECTRA
ACOUSTIC TOMOGRAPHY
MELTING
TOMOGRAPHY
SEA LEVEL
ROSS SEA
ARCTIC OCEAN
MONITORING
POLAR REGIONS
ICE
ARCTIC OCEANOGRAPHY
CAPILLARIES
OCEAN SURFACE ROUGHNESS
POLAR ICE
SEA LEVEL RISE
WIND DRAG
spellingShingle Physical and Dynamic Oceanography
*OCEAN SURFACE
*GRAVITY WAVES
WIND
BIBLIOGRAPHIES
SPECTRA
ACOUSTIC TOMOGRAPHY
MELTING
TOMOGRAPHY
SEA LEVEL
ROSS SEA
ARCTIC OCEAN
MONITORING
POLAR REGIONS
ICE
ARCTIC OCEANOGRAPHY
CAPILLARIES
OCEAN SURFACE ROUGHNESS
POLAR ICE
SEA LEVEL RISE
WIND DRAG
Munk, Walter
Secretary of the Navy Professor of Oceanography
topic_facet Physical and Dynamic Oceanography
*OCEAN SURFACE
*GRAVITY WAVES
WIND
BIBLIOGRAPHIES
SPECTRA
ACOUSTIC TOMOGRAPHY
MELTING
TOMOGRAPHY
SEA LEVEL
ROSS SEA
ARCTIC OCEAN
MONITORING
POLAR REGIONS
ICE
ARCTIC OCEANOGRAPHY
CAPILLARIES
OCEAN SURFACE ROUGHNESS
POLAR ICE
SEA LEVEL RISE
WIND DRAG
description The principal research effort has been towards understanding the high-frequency tail of the surface gravity wave spectrum, lengths of 2 cm to 60 cm; these a principally responsible for wind drag on water. Analysis was based on a unique data set from geophones and hydrophones at 5 1/2 km depth midway between California and Hawaii. The measured spectral intensity around 10 Hz gives a more accurate measure of local winds than the standard satellite scatterometry. A spectral gap at the 30 Hz gravity to capillary transition offers new opportunities for spectral monitoring. We are making progress towards understanding the generation processes A continuing effort towards the acoustic monitoring of ocean processes has been directed at the polar ocean cavities sandwiched between the floating ice sheet and the sea floor. We are exploring a possible tomography experiment in the Ross Sea with the goal of better predicting polar ice melting processes and the associated global rise in sea level.
author2 SCRIPPS INSTITUTION OF OCEANOGRAPHY LA JOLLA CA
format Text
author Munk, Walter
author_facet Munk, Walter
author_sort Munk, Walter
title Secretary of the Navy Professor of Oceanography
title_short Secretary of the Navy Professor of Oceanography
title_full Secretary of the Navy Professor of Oceanography
title_fullStr Secretary of the Navy Professor of Oceanography
title_full_unstemmed Secretary of the Navy Professor of Oceanography
title_sort secretary of the navy professor of oceanography
publishDate 2011
url http://www.dtic.mil/docs/citations/ADA542691
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA542691
geographic Arctic
Arctic Ocean
Ross Sea
geographic_facet Arctic
Arctic Ocean
Ross Sea
genre Arctic
Arctic Ocean
Ice Sheet
Ross Sea
genre_facet Arctic
Arctic Ocean
Ice Sheet
Ross Sea
op_source DTIC
op_relation http://www.dtic.mil/docs/citations/ADA542691
op_rights Approved for public release; distribution is unlimited.
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