Long Wave Coupling of the Mid and South Atlantic Bights Forced by the Atmosphere
The eastern United States continental margin profile is relatively uniform throughout the Middle Atlantic Bight (Hatteras to Gulf of Maine), but in the South Atlantic Bight (Florida Keys to Hatteras) it bifurcates into an inner and outer slope region. Coastal tide gage records indicate that sea leve...
Main Author: | |
---|---|
Other Authors: | |
Format: | Text |
Language: | English |
Published: |
1979
|
Subjects: | |
Online Access: | http://www.dtic.mil/docs/citations/ADA072282 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA072282 |
id |
ftdtic:ADA072282 |
---|---|
record_format |
openpolar |
spelling |
ftdtic:ADA072282 2023-05-15T17:34:14+02:00 Long Wave Coupling of the Mid and South Atlantic Bights Forced by the Atmosphere Brooks,David A TEXAS A AND M UNIV COLLEGE STATION DEPT OF OCEANOGRAPHY 1979-05 text/html http://www.dtic.mil/docs/citations/ADA072282 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA072282 en eng http://www.dtic.mil/docs/citations/ADA072282 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Meteorology Physical and Dynamic Oceanography *OCEAN WAVES *AIR WATER INTERACTIONS *SEA LEVEL COUPLING(INTERACTION) UNITED STATES SURFACE WAVES DYNAMIC RESPONSE WIND TIME SERIES ANALYSIS REGRESSION ANALYSIS OCEANOGRAPHIC DATA CONTINENTAL SHELVES CONTINENTAL SLOPES SEASONAL VARIATIONS BAROMETRIC PRESSURE LONG WAVELENGTHS SPECTRUM ANALYSIS GULF STREAM NORTH ATLANTIC OCEAN OCEAN BOTTOM TOPOGRAPHY HEIGHT PERIODIC VARIATIONS OCEAN TIDES MARINE GEOPHYSICS Barotropic waves Text 1979 ftdtic 2016-02-20T16:36:31Z The eastern United States continental margin profile is relatively uniform throughout the Middle Atlantic Bight (Hatteras to Gulf of Maine), but in the South Atlantic Bight (Florida Keys to Hatteras) it bifurcates into an inner and outer slope region. Coastal tide gage records indicate that sea level oscillations with periods longer than one week can propagate southward as continental shelf waves in both Bights, thereby providing a coupling mechanism between the Bights. However, several-day period motions appear to be confined to the South Atlantic Bight and may result from backscattering of long wave energy by the variable topography and the Gulf Stream. The coastal sea level phase data for the several-day period motions is not easily attributable to a monochromatic propagating wave; rather, it appears that wave group properties may lead to a more consistent explanation of the phases. Cross-shelf and longshelf wind stress components were both strongly coupled to sea level fluctuations for long periods; short period motions were more closely associated with dynamic responses to atmospheric pressure fluctuations. Text North Atlantic Defense Technical Information Center: DTIC Technical Reports database Gage ENVELOPE(-118.503,-118.503,56.133,56.133) |
institution |
Open Polar |
collection |
Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
Meteorology Physical and Dynamic Oceanography *OCEAN WAVES *AIR WATER INTERACTIONS *SEA LEVEL COUPLING(INTERACTION) UNITED STATES SURFACE WAVES DYNAMIC RESPONSE WIND TIME SERIES ANALYSIS REGRESSION ANALYSIS OCEANOGRAPHIC DATA CONTINENTAL SHELVES CONTINENTAL SLOPES SEASONAL VARIATIONS BAROMETRIC PRESSURE LONG WAVELENGTHS SPECTRUM ANALYSIS GULF STREAM NORTH ATLANTIC OCEAN OCEAN BOTTOM TOPOGRAPHY HEIGHT PERIODIC VARIATIONS OCEAN TIDES MARINE GEOPHYSICS Barotropic waves |
spellingShingle |
Meteorology Physical and Dynamic Oceanography *OCEAN WAVES *AIR WATER INTERACTIONS *SEA LEVEL COUPLING(INTERACTION) UNITED STATES SURFACE WAVES DYNAMIC RESPONSE WIND TIME SERIES ANALYSIS REGRESSION ANALYSIS OCEANOGRAPHIC DATA CONTINENTAL SHELVES CONTINENTAL SLOPES SEASONAL VARIATIONS BAROMETRIC PRESSURE LONG WAVELENGTHS SPECTRUM ANALYSIS GULF STREAM NORTH ATLANTIC OCEAN OCEAN BOTTOM TOPOGRAPHY HEIGHT PERIODIC VARIATIONS OCEAN TIDES MARINE GEOPHYSICS Barotropic waves Brooks,David A Long Wave Coupling of the Mid and South Atlantic Bights Forced by the Atmosphere |
topic_facet |
Meteorology Physical and Dynamic Oceanography *OCEAN WAVES *AIR WATER INTERACTIONS *SEA LEVEL COUPLING(INTERACTION) UNITED STATES SURFACE WAVES DYNAMIC RESPONSE WIND TIME SERIES ANALYSIS REGRESSION ANALYSIS OCEANOGRAPHIC DATA CONTINENTAL SHELVES CONTINENTAL SLOPES SEASONAL VARIATIONS BAROMETRIC PRESSURE LONG WAVELENGTHS SPECTRUM ANALYSIS GULF STREAM NORTH ATLANTIC OCEAN OCEAN BOTTOM TOPOGRAPHY HEIGHT PERIODIC VARIATIONS OCEAN TIDES MARINE GEOPHYSICS Barotropic waves |
description |
The eastern United States continental margin profile is relatively uniform throughout the Middle Atlantic Bight (Hatteras to Gulf of Maine), but in the South Atlantic Bight (Florida Keys to Hatteras) it bifurcates into an inner and outer slope region. Coastal tide gage records indicate that sea level oscillations with periods longer than one week can propagate southward as continental shelf waves in both Bights, thereby providing a coupling mechanism between the Bights. However, several-day period motions appear to be confined to the South Atlantic Bight and may result from backscattering of long wave energy by the variable topography and the Gulf Stream. The coastal sea level phase data for the several-day period motions is not easily attributable to a monochromatic propagating wave; rather, it appears that wave group properties may lead to a more consistent explanation of the phases. Cross-shelf and longshelf wind stress components were both strongly coupled to sea level fluctuations for long periods; short period motions were more closely associated with dynamic responses to atmospheric pressure fluctuations. |
author2 |
TEXAS A AND M UNIV COLLEGE STATION DEPT OF OCEANOGRAPHY |
format |
Text |
author |
Brooks,David A |
author_facet |
Brooks,David A |
author_sort |
Brooks,David A |
title |
Long Wave Coupling of the Mid and South Atlantic Bights Forced by the Atmosphere |
title_short |
Long Wave Coupling of the Mid and South Atlantic Bights Forced by the Atmosphere |
title_full |
Long Wave Coupling of the Mid and South Atlantic Bights Forced by the Atmosphere |
title_fullStr |
Long Wave Coupling of the Mid and South Atlantic Bights Forced by the Atmosphere |
title_full_unstemmed |
Long Wave Coupling of the Mid and South Atlantic Bights Forced by the Atmosphere |
title_sort |
long wave coupling of the mid and south atlantic bights forced by the atmosphere |
publishDate |
1979 |
url |
http://www.dtic.mil/docs/citations/ADA072282 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA072282 |
long_lat |
ENVELOPE(-118.503,-118.503,56.133,56.133) |
geographic |
Gage |
geographic_facet |
Gage |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/ADA072282 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
_version_ |
1766133009452367872 |