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  • 1
    Online Resource
    Online Resource
    Mississippi River flood waters that reached the Gulf Stream
    American Geophysical Union (AGU) ; 1995
    In:  Journal of Geophysical Research: Oceans Vol. 100, No. C7 ( 1995-07-15), p. 13595-13601
    Details
    In: Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 100, No. C7 ( 1995-07-15), p. 13595-13601
    Abstract: Distributions of physical, biological, and chemical parameters in Florida Keys coastal waters seaward of the reef track were surveyed on September 9 to 13, 1993, as part of a coordinated multidisciplinary study of surface transport processes. A band of low‐salinity water was observed along the shoreward side of the Florida Current over the downstream extent of the survey from Miami to Key West. Biological and chemical indicators within the band, together with its large volume, satellite imagery, and a surface drifter trajectory suggested the recent Mississippi River flood as the source.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    URL: Article
    DOI: 10.1029/95JC01039
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1995
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    SSG: 16,13
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    Online Resource
  • 2
    Online Resource
    Online Resource
    Observations of a Gulf Stream frontal eddy on the Georgia continental shelf, April 1977
    Elsevier BV ; 1981
    In:  Deep Sea Research Part A. Oceanographic Research Papers Vol. 28, No. 4 ( 1981-4), p. 347-378
    Details
    In: Deep Sea Research Part A. Oceanographic Research Papers, Elsevier BV, Vol. 28, No. 4 ( 1981-4), p. 347-378
    Type of Medium: Online Resource
    ISSN: 0198-0149
    URL: Article
    DOI: 10.1016/0198-0149(81)90004-2
    Language: English
    Publisher: Elsevier BV
    Publication Date: 1981
    detail.hit.zdb_id: 2280519-9
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  • 3
    Online Resource
    Online Resource
    A bottom water intrusion in Onslow Bay, North Carolina
    Elsevier BV ; 1981
    In:  Deep Sea Research Part A. Oceanographic Research Papers Vol. 28, No. 4 ( 1981-4), p. 329-345
    Details
    In: Deep Sea Research Part A. Oceanographic Research Papers, Elsevier BV, Vol. 28, No. 4 ( 1981-4), p. 329-345
    Type of Medium: Online Resource
    ISSN: 0198-0149
    URL: Article
    DOI: 10.1016/0198-0149(81)90003-0
    Language: English
    Publisher: Elsevier BV
    Publication Date: 1981
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  • 4
    Online Resource
    Online Resource
    On the predictability of high water level along the US East Coast: can the Florida Current measurement be an indicator for flooding caused by remote forcing?
    Springer Science and Business Media LLC ; 2017
    In:  Ocean Dynamics Vol. 67, No. 6 ( 2017-6), p. 751-766
    Details
    In: Ocean Dynamics, Springer Science and Business Media LLC, Vol. 67, No. 6 ( 2017-6), p. 751-766
    Type of Medium: Online Resource
    ISSN: 1616-7341 , 1616-7228
    URL: Article
    DOI: 10.1007/s10236-017-1057-0
    Language: English
    Publisher: Springer Science and Business Media LLC
    Publication Date: 2017
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    SSG: 14
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  • 5
    Online Resource
    Online Resource
    Climatology of the southeastern United States continental shelf waters
    American Geophysical Union (AGU) ; 1983
    In:  Journal of Geophysical Research: Oceans Vol. 88, No. C8 ( 1983-05-30), p. 4705-4718
    Details
    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
    URL: Article
    DOI: 10.1029/JC088iC08p04705
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1983
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  • 6
    Online Resource
    Online Resource
    Distribution of Antarctic intermediate water over the Blake Plateau
    American Geophysical Union (AGU) ; 1983
    In:  Journal of Geophysical Research: Oceans Vol. 88, No. C8 ( 1983-05-30), p. 4699-4704
    Details
    In: Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 88, No. C8 ( 1983-05-30), p. 4699-4704
    Abstract: During a cruise in September 1980 over the Blake Plateau we observed a northward spread of Antarctic Intermediate Water (AAIW) in the main axis of the Gulf Stream. The AAIW appeared as a lobe less than 60 km wide extending to at least 31°N. The lobe was characterized by negative salinity anomalies of 0.15×10 −3 , elevated nutrient concentrations, and lowered oxygen concentrations. Tentative evidence suggests that a parcel of AAIW was located over the central Blake Plateau, and geostrophic calculations indicate it may have been attached to the main Gulf Stream deep flow.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    URL: Article
    DOI: 10.1029/JC088iC08p04699
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1983
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    SSG: 16,13
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  • 7
    Online Resource
    Online Resource
    A note on the Charleston Gyre
    American Geophysical Union (AGU) ; 1985
    In:  Journal of Geophysical Research: Oceans Vol. 90, No. C6 ( 1985-11-20), p. 11857-11861
    Details
    In: Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 90, No. C6 ( 1985-11-20), p. 11857-11861
    Abstract: The deflection of the Gulf Stream caused by a topographic feature—the Charleston Bump, located offshore of Savannah, Georgia—results in a quasi‐stationary cyclonic eddy—the Charleston Gyre which is situated over the continental slope east of Charleston and Cape Romain. Occasionally, the upwelling associated with this eddy produces an enhancement in the surface layer primary production that is great enough to be detected by the Nimbus 7 coastal zone color scanner (CZCS). In this note a CZCS image with simultaneous hydrography, current, and wind observations is presented that documents an unusual manifestation of the gyre. In addition to the CZCS image a Seasat synthetic aperture radar (SAR) image is included that clearly indicates the presence of the eddy adjacent to the Gulf Stream front.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    URL: Article
    DOI: 10.1029/JC090iC06p11857
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1985
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    SSG: 16,13
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  • 8
    Online Resource
    Online Resource
    Gulf Stream frontal eddy influence on productivity of the southeast U.S. continental shelf
    American Geophysical Union (AGU) ; 1991
    In:  Journal of Geophysical Research: Oceans Vol. 96, No. C12 ( 1991-12-15), p. 22191-22205
    Details
    In: Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 96, No. C12 ( 1991-12-15), p. 22191-22205
    Abstract: Weekly period meanders and eddies are persistent features of Gulf Stream frontal dynamics from Miami, Florida, to Cape Hatteras, North Carolina. Satellite imagery and moored current and temperature records reveal a spatial pattern of preferred regions for growth and decay of frontal disturbances. Growth regions occur off Miami, Cape Canaveral, and Cape Fear due to baroclinic instability, and decay occurs in the confines of the Straits of Florida between Miami and Palm Beach, between 30° and 32°N where the stream approaches the topographic feature known as the Charleston bump and between 33°N and Cape Hatteras. Eddy decay regions are associated with elongation of frontal features, offshore transport of momentum and heat, and onshore transport of nutrients. Onshore transport of new nitrogen from the nutrient‐bearing strata beneath the Gulf Stream indicates that frontal eddies serve as a “nutrient pump” for the shelf. New nitrogen flux to the shelf due to Gulf Stream input could support new production of 7.4×10 12 g C yr −1 or about 8 million tons carbon per year if all nitrate were utilized. Calculations indicate that approximately 70% of this potential new production is realized, yielding an annual new production for the outer shelf of 4.3×10 12 g C.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    URL: Article
    DOI: 10.1029/91JC02450
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1991
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    SSG: 16,13
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  • 9
    Online Resource
    Online Resource
    Effect of air bubble solution on air-sea gas exchange
    American Geophysical Union (AGU) ; 1973
    In:  Journal of Geophysical Research Vol. 78, No. 6 ( 1973-02-20), p. 962-968
    Details
    In: Journal of Geophysical Research, American Geophysical Union (AGU), Vol. 78, No. 6 ( 1973-02-20), p. 962-968
    Type of Medium: Online Resource
    ISSN: 0148-0227
    URL: Article
    DOI: 10.1029/JC078i006p00962
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1973
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    SSG: 16,13
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  • 10
    Online Resource
    Online Resource
    A time-dependent model of nutrient distribution in continental shelf waters
    Elsevier BV ; 1980
    In:  Ecological Modelling Vol. 10, No. 3-4 ( 1980-8), p. 193-214
    Details
    In: Ecological Modelling, Elsevier BV, Vol. 10, No. 3-4 ( 1980-8), p. 193-214
    Type of Medium: Online Resource
    ISSN: 0304-3800
    URL: Article
    DOI: 10.1016/0304-3800(80)90059-9
    RVK:
    AR 10100
    Language: English
    Publisher: Elsevier BV
    Publication Date: 1980
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    detail.hit.zdb_id: 2000879-X
    SSG: 12
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