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  • 1
    Online Resource
    Online Resource
    Elsevier BV ; 2008
    In:  Estuarine, Coastal and Shelf Science Vol. 78, No. 1 ( 2008-6), p. 190-202
    In: Estuarine, Coastal and Shelf Science, Elsevier BV, Vol. 78, No. 1 ( 2008-6), p. 190-202
    Type of Medium: Online Resource
    ISSN: 0272-7714
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2008
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  • 2
    Online Resource
    Online Resource
    Elsevier BV ; 2002
    In:  Continental Shelf Research Vol. 22, No. 11-13 ( 2002-07), p. 1731-1743
    In: Continental Shelf Research, Elsevier BV, Vol. 22, No. 11-13 ( 2002-07), p. 1731-1743
    Type of Medium: Online Resource
    ISSN: 0278-4343
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2002
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  • 3
    In: Continental Shelf Research, Elsevier BV, Vol. 4, No. 6 ( 1985-1), p. 611-635
    Type of Medium: Online Resource
    ISSN: 0278-4343
    Language: English
    Publisher: Elsevier BV
    Publication Date: 1985
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  • 4
    Online Resource
    Online Resource
    American Meteorological Society ; 1981
    In:  Journal of Physical Oceanography Vol. 11, No. 12 ( 1981-12), p. 1627-1637
    In: Journal of Physical Oceanography, American Meteorological Society, Vol. 11, No. 12 ( 1981-12), p. 1627-1637
    Type of Medium: Online Resource
    ISSN: 0022-3670 , 1520-0485
    Language: English
    Publisher: American Meteorological Society
    Publication Date: 1981
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  • 5
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1996
    In:  Journal of Geophysical Research: Oceans Vol. 101, No. C6 ( 1996-06-15), p. 14253-14268
    In: Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 101, No. C6 ( 1996-06-15), p. 14253-14268
    Abstract: The circulation in the vicinity of an idealized tidal inlet connecting a continental shelf and a coastal sound is examined. The circulation is forced by an M 2 tide and a weakly buoyant discharge. The buoyant discharge forms a plume in the coastal ocean and induces a distinct anticyclonic circulation at the plume edge that is maintained throughout the tidal cycle. We focus on the plume's onset and its evolution over 5–10 tidal cycles. Over the timescales considered, the plume was roughly circular, slightly skewed in the along‐coast direction. The model solution yielded high vertical Ekman numbers E ϵ ∼ O (5) in the vicinity of the inlet mouth, decreasing seaward from the inlet to an order of magnitude smaller ( E ϵ ∼ 0.25) at the seaward edge of the plume. Passive particles released in the region seaward of the inlet mouth were used to describe the exchange between the coastal region and the inlet. A marked asymmetry between ebb and flood flows is observed in the vicinity of the inlet, with jet‐like ebbing currents and weaker potential‐flow‐like flooding currents. Over a tidal cycle, net exchanges between the coastal ocean and the inlet are found to be spatially and temporally dependent; that is, particle trajectories depend on the release point and the time of the release in the tidal cycle. The near‐inlet residual circulation shows significant differences in the absence of stratification.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1996
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    detail.hit.zdb_id: 3094268-8
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  • 6
    Online Resource
    Online Resource
    Wiley ; 1973
    In:  Limnology and Oceanography Vol. 18, No. 5 ( 1973-09), p. 697-704
    In: Limnology and Oceanography, Wiley, Vol. 18, No. 5 ( 1973-09), p. 697-704
    Type of Medium: Online Resource
    ISSN: 0024-3590
    Language: English
    Publisher: Wiley
    Publication Date: 1973
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  • 7
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1983
    In:  Journal of Geophysical Research: Oceans Vol. 88, No. C8 ( 1983-05-30), p. 4705-4718
    In: Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 88, No. C8 ( 1983-05-30), p. 4705-4718
    Abstract: Data from 2872 hydrographic stations have been used to determine the oceanographie climatology of the southeastern United States continental shelf waters. The data were sorted by each degree of latitude and by depth into three zones (0–20 m, 21–40 m, 41–60 m). Inner shelf water temperatures were similar to adjacent land air temperatures, while outer shelf temperatures were moderated by the Gulf Stream. Minimum and maximum water temperatures occurred in Georgia and South Carolina inner shelf water. Bottom temperatures were unusually low off Florida in the summer probably because of shelf break upwelling. Surface salinity was lowest adjacent to the rivers and reached minimums in the spring at the time of high runoff. An exception to this occurred in the fall, when strong southward winds apparently advected low salinity coastal water southward and offshore flow was restricted. Heat flux was calculated from changes in monthly mean depth‐averaged inner shelf water temperatures. Heating occurred from March through July with maximum rates of 103 W m −2 . Cooling occurred from October through February with maximum rates of −90 W m −2 . Bulk stratification was estimated from the difference in near‐surface and near‐bottom monthly mean density. In the spring, stratification increases in inner shelf areas because of decreasing winds and increasing heat flux and runoff. By summer the whole shelf is highly stratified reflecting the contrast between high surface water temperatures and cooler bottom waters. Highest bulk stratification is found over the outer shelf. Stratification decreased with the approach offall with the associated cooling and high winds. Mean flow at midshelf was northward and appears to be produced by an along‐shelf slope of sea level of oceanic origin. Data are available with entire article on microfiche. Order from the American Geophysical Union, 2000 Florida Avenue, N.W. Washington, D.C. 20009. Document C82‐002; $2.50. Payment must accompany order.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1983
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    detail.hit.zdb_id: 3094268-8
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    detail.hit.zdb_id: 3094181-7
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  • 8
    Online Resource
    Online Resource
    American Meteorological Society ; 1985
    In:  Journal of Physical Oceanography Vol. 15, No. 12 ( 1985-12), p. 1733-1746
    In: Journal of Physical Oceanography, American Meteorological Society, Vol. 15, No. 12 ( 1985-12), p. 1733-1746
    Type of Medium: Online Resource
    ISSN: 0022-3670 , 1520-0485
    Language: English
    Publisher: American Meteorological Society
    Publication Date: 1985
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  • 9
    Online Resource
    Online Resource
    American Meteorological Society ; 1987
    In:  Journal of Physical Oceanography Vol. 17, No. 12 ( 1987-12), p. 2318-2333
    In: Journal of Physical Oceanography, American Meteorological Society, Vol. 17, No. 12 ( 1987-12), p. 2318-2333
    Type of Medium: Online Resource
    ISSN: 0022-3670 , 1520-0485
    Language: English
    Publisher: American Meteorological Society
    Publication Date: 1987
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  • 10
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1989
    In:  Journal of Geophysical Research: Oceans Vol. 94, No. C8 ( 1989-08-15), p. 10686-10698
    In: Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 94, No. C8 ( 1989-08-15), p. 10686-10698
    Abstract: Data collected during winter from a set of offshore buoys and coastal meteorological stations on the continental shelf of the southeastern United States were analyzed as part of a meteorological and oceanographic study of the genesis of winter cyclones (Project GALE). The analyses were designed to describe the temporal and spatial variability of wind stress and heat flux over the shelf. While there were some episodes of strong spatial variations in wind stress, the wind field, on the whole, was remarkably uniform. Largest gradients were associated with times immediately preceding outbreaks of cold continental air over the shelf. Maximum heat fluxes occurred during these cold air outbreaks and reached as high as 1400 W/ m 2 on the outer shelf near the Gulf Stream. The largest wind stress values occurred in the cross‐shelf component and reached 0.7 Pa. The cross‐shelf wind was highly correlated with the geostrophic wind, but there were significant ageostrophic deviations in the alongshelf component. These deviations were correlated with fluctuations in sea‐air temperature differences. The fluctuations in heat flux are thought to modulate the alongshelf component by inducing added vorticity in the planetary boundary layer over the scale width of the continental shelf.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1989
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