Topographic Influence on Internal Waves and Mesoscale Oceanic Dynamics, Including Lateral and Vertical Mixing in Marginal Zones of North Atlantic

The long-term goal of our research is to identify and quantify key processes responsible for vertical and lateral mixing in oceans, which influences transports of heat, energy, momentum, dissolved matter and plankton in pelagic and littoral oceans. The main objective of the project is to conduct a c...

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Main Authors: Lozovatsky, Iossif, Fernando, Harindra J
Other Authors: ARIZONA STATE UNIV TEMPE DEPT OF MECHANICAL AND AEROSPACE ENGINEERING
Format: Text
Language:English
Published: 2001
Subjects:
Online Access:http://www.dtic.mil/docs/citations/ADA623162
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA623162
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spelling ftdtic:ADA623162 2023-05-15T17:29:55+02:00 Topographic Influence on Internal Waves and Mesoscale Oceanic Dynamics, Including Lateral and Vertical Mixing in Marginal Zones of North Atlantic Lozovatsky, Iossif Fernando, Harindra J ARIZONA STATE UNIV TEMPE DEPT OF MECHANICAL AND AEROSPACE ENGINEERING 2001-09-30 text/html http://www.dtic.mil/docs/citations/ADA623162 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA623162 en eng http://www.dtic.mil/docs/citations/ADA623162 Approved for public release; distribution is unlimited. DTIC Physical and Dynamic Oceanography *INTERNAL WAVES *OCEAN BOTTOM TOPOGRAPHY ENERGY TRANSFER HEAT TRANSFER MIXING MOMENTUM NORTH ATLANTIC OCEAN PLANKTON DISSOLVED MATTER MARGINAL ZONES MESOSCALE OCEANIC DYNAMICS Text 2001 ftdtic 2016-02-24T19:06:21Z The long-term goal of our research is to identify and quantify key processes responsible for vertical and lateral mixing in oceans, which influences transports of heat, energy, momentum, dissolved matter and plankton in pelagic and littoral oceans. The main objective of the project is to conduct a comprehensive analysis of small and mesoscale phenomena, focusing on oceanic marginal zones. Mixing, internal waves and transformation of water masses were of major concern during the last year. We continued the development of a web-accessible database containing mooring and profiling measurements taken by Russian oceanographers in deep basins of the Atlantic, Pacific, and Indian oceans, at trans-Atlantic sections and in the marginal seas of western Pacific. Collection of new data pertinent to turbulent mixing in the near-surface boundary layers, both from oceanic and atmospheric sides, was an important part of our work. Text North Atlantic Defense Technical Information Center: DTIC Technical Reports database Indian Pacific
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Physical and Dynamic Oceanography
*INTERNAL WAVES
*OCEAN BOTTOM TOPOGRAPHY
ENERGY TRANSFER
HEAT TRANSFER
MIXING
MOMENTUM
NORTH ATLANTIC OCEAN
PLANKTON
DISSOLVED MATTER
MARGINAL ZONES
MESOSCALE OCEANIC DYNAMICS
spellingShingle Physical and Dynamic Oceanography
*INTERNAL WAVES
*OCEAN BOTTOM TOPOGRAPHY
ENERGY TRANSFER
HEAT TRANSFER
MIXING
MOMENTUM
NORTH ATLANTIC OCEAN
PLANKTON
DISSOLVED MATTER
MARGINAL ZONES
MESOSCALE OCEANIC DYNAMICS
Lozovatsky, Iossif
Fernando, Harindra J
Topographic Influence on Internal Waves and Mesoscale Oceanic Dynamics, Including Lateral and Vertical Mixing in Marginal Zones of North Atlantic
topic_facet Physical and Dynamic Oceanography
*INTERNAL WAVES
*OCEAN BOTTOM TOPOGRAPHY
ENERGY TRANSFER
HEAT TRANSFER
MIXING
MOMENTUM
NORTH ATLANTIC OCEAN
PLANKTON
DISSOLVED MATTER
MARGINAL ZONES
MESOSCALE OCEANIC DYNAMICS
description The long-term goal of our research is to identify and quantify key processes responsible for vertical and lateral mixing in oceans, which influences transports of heat, energy, momentum, dissolved matter and plankton in pelagic and littoral oceans. The main objective of the project is to conduct a comprehensive analysis of small and mesoscale phenomena, focusing on oceanic marginal zones. Mixing, internal waves and transformation of water masses were of major concern during the last year. We continued the development of a web-accessible database containing mooring and profiling measurements taken by Russian oceanographers in deep basins of the Atlantic, Pacific, and Indian oceans, at trans-Atlantic sections and in the marginal seas of western Pacific. Collection of new data pertinent to turbulent mixing in the near-surface boundary layers, both from oceanic and atmospheric sides, was an important part of our work.
author2 ARIZONA STATE UNIV TEMPE DEPT OF MECHANICAL AND AEROSPACE ENGINEERING
format Text
author Lozovatsky, Iossif
Fernando, Harindra J
author_facet Lozovatsky, Iossif
Fernando, Harindra J
author_sort Lozovatsky, Iossif
title Topographic Influence on Internal Waves and Mesoscale Oceanic Dynamics, Including Lateral and Vertical Mixing in Marginal Zones of North Atlantic
title_short Topographic Influence on Internal Waves and Mesoscale Oceanic Dynamics, Including Lateral and Vertical Mixing in Marginal Zones of North Atlantic
title_full Topographic Influence on Internal Waves and Mesoscale Oceanic Dynamics, Including Lateral and Vertical Mixing in Marginal Zones of North Atlantic
title_fullStr Topographic Influence on Internal Waves and Mesoscale Oceanic Dynamics, Including Lateral and Vertical Mixing in Marginal Zones of North Atlantic
title_full_unstemmed Topographic Influence on Internal Waves and Mesoscale Oceanic Dynamics, Including Lateral and Vertical Mixing in Marginal Zones of North Atlantic
title_sort topographic influence on internal waves and mesoscale oceanic dynamics, including lateral and vertical mixing in marginal zones of north atlantic
publishDate 2001
url http://www.dtic.mil/docs/citations/ADA623162
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA623162
geographic Indian
Pacific
geographic_facet Indian
Pacific
genre North Atlantic
genre_facet North Atlantic
op_source DTIC
op_relation http://www.dtic.mil/docs/citations/ADA623162
op_rights Approved for public release; distribution is unlimited.
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