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Articles 1471 - 1500 of 2567
Full-Text Articles in Entire DC Network
Spatial Patterns Of Grazing-Related Parameters In California Coastal Surface Waters, July 1979, James L. Cox, Loren R. Haury, James J. Simpson
Spatial Patterns Of Grazing-Related Parameters In California Coastal Surface Waters, July 1979, James L. Cox, Loren R. Haury, James J. Simpson
Journal of Marine Research
A surface survey using underway continuous mapping of temperature, chlorophyll, zooplankton (>153 µm) wet weight density, and activity of the zooplankton digestive enzyme laminarinase was undertaken for a 20-day period during active upwelling in the California coastal region between Pt. Arena and Pt. Conception, California, U.S.A., during July, 1979....
Radionuclides From Windscale Discharges Ii: Their Dispersion In Scottish And Norwegian Coastal Circulation, Hugh D. Livingston, Vaughan T. Bowen, Stuart L. Kupferman
Radionuclides From Windscale Discharges Ii: Their Dispersion In Scottish And Norwegian Coastal Circulation, Hugh D. Livingston, Vaughan T. Bowen, Stuart L. Kupferman
Journal of Marine Research
Measurement of the concentrations of 134Cs, 137Cs, 90Sr, 238Pu, and 239, 240Pu in Scottish and Norwegian coastal waters in 1976 and 1978 provides information on dispersal pathways, transport times, and dilution in these waters of radioactive waste discharged to the Irish Sea from the Windscale nuclear fuel reprocessing plant in Cumbria, U. K....
The Worthington Effect And The Origin Of The Younger Dryas, W. H. Berger, J. S. Killingley
The Worthington Effect And The Origin Of The Younger Dryas, W. H. Berger, J. S. Killingley
Journal of Marine Research
An increase in CO2 content of the atmosphere during deglaciation is explained by buildup of shelf carbonate with concomitant release of "excess CO2" to the surrounding upper ocean, from whence some of it enters the atmosphere. Mixing with deep water removes excess CO2 to the abyss where it is used up in dissolving foraminifera and coccoliths....
A Note On The Heat Balance Of The Mediterranean And Red Seas, A. F. Bunker, H. Charnock, R. A. Goldsmith
A Note On The Heat Balance Of The Mediterranean And Red Seas, A. F. Bunker, H. Charnock, R. A. Goldsmith
Journal of Marine Research
The Mediterranean and Red Seas are used as test volumes in an attempt to assess the accuracy of estimates of climatological air-sea fluxes calculated using meteorological observations from merchant ships….
Origin Of The Mediterranean Outflow, Harry L. Bryden, Henry M. Stommel
Origin Of The Mediterranean Outflow, Harry L. Bryden, Henry M. Stommel
Journal of Marine Research
Toe origin of the Mediterranean outflow is one of oceanography's oldest problems. In this work, the flow of western Mediterranean deep water up and over the sill at Gibraltar is investigated from hydrographic observations and current measurements. The deep water is found to flow westward along the Moroccan continental slope in the western Mediterranean or Alboran Sea and to rise as it approaches the Strait of Gibraltar....
The Antarctic Circumpolar Current And The Oceanic Heat And Freshwater Budgets, Daniel T. Georgi, John M. Toole
The Antarctic Circumpolar Current And The Oceanic Heat And Freshwater Budgets, Daniel T. Georgi, John M. Toole
Journal of Marine Research
Hydrographic sections that span the Antarctic Circumpolar Current are used to estimate the zonal heat and freshwater transports south of Africa, New Zealand and America. These in tum are used to calculate the exchanges of heat and freshwater between the three major oceans....
On The Transport And Modification Of Antarctic Bottom Water In The Vema Channel, Nelson Hogg, Pierre Biscaye, Wilford Gardner, William J. Schmitz Jr.
On The Transport And Modification Of Antarctic Bottom Water In The Vema Channel, Nelson Hogg, Pierre Biscaye, Wilford Gardner, William J. Schmitz Jr.
Journal of Marine Research
The Verna Channel is a deep passage across the Rio Grande Rise in the South Atlantic through which Antarctic Bottom Water (AABW) must flow on its way northward from the Argentine Basin to the Brazil Basin and eventuafly into the North Atlantic….
Response Of The Western Equatorial Atlantic Ocean To An Annual Wind Cycle, Eli Joel Katz, Silvia Garzoli
Response Of The Western Equatorial Atlantic Ocean To An Annual Wind Cycle, Eli Joel Katz, Silvia Garzoli
Journal of Marine Research
From the Global Weather Experiment in 1979, four one-year data records are juxtaposed which simultaneously describe the wind stress, thermocline depth, surface current and transport of the Equatorial Undercurrent in the western equatorial Atlantic….
Seasonal Variability Of Temperature And Salinity In The Labrador Current, John R.N. Lazier
Seasonal Variability Of Temperature And Salinity In The Labrador Current, John R.N. Lazier
Journal of Marine Research
Most of the available temperature and salinity data from the waters above the Labrador continental shelf and slope are assembled and analyzed for seasonal variations. It is first demonstrated that the horizontal temperature and salinity gradients are small in the waters over the shelf relative to the gradients across the slope where the strongest part of the Labrador Current is trapped....
The Subtropical Recirculation Of Mode Waters, Michael S. Mccartney
The Subtropical Recirculation Of Mode Waters, Michael S. Mccartney
Journal of Marine Research
A "Mode Water" is a particular type of water mass characterized by its vertical homogeneity. There are two general varieties in the world ocean: Subtropical Mode Waters and Subpolar Mode Waters. The vertical homogeneity of a Mode Water is acquired by the process of deep vertical convection in winter. The low vertical density gradient imparted to the water column by convection persists laterally as the general circulation carries the Mode Water away from the formation zone....
Walter Hoxton's 1735 Description Of The Gulf Stream, P. L. Richardson
Walter Hoxton's 1735 Description Of The Gulf Stream, P. L. Richardson
Journal of Marine Research
In 1735 Walter Hoxton, on his chart of Chesapeake Bay, gave an early and accurate description of the western Gulf Stream. Hoxton's pioneering measurements by ship-drift of the mean limits, direction and speed of the Gulf Stream were the first to show that the Stream is a narrow, swift boundary current which leaves the coast near Cape Hatteras. and turns eastward near 38N latitude. The Hoxton description of the Stream antedates by 35 years the Franklin-Folger chart of the Stream.
The Kinematic And Thermohaline Zonation Of The Antarctic Circumpolar Current At Drake Passage, Worth D. Nowlin Jr., Melody Clifford
The Kinematic And Thermohaline Zonation Of The Antarctic Circumpolar Current At Drake Passage, Worth D. Nowlin Jr., Melody Clifford
Journal of Marine Research
The waters of the Antarctic Circumpolar Current at Drake Passage show mesoscale horizontal zonation into four water mass regimes horizontally separated by three fronts. Vertical profiles of T, S and O2 on opposite sides of each front are described and compared. Although the surface waters are significantly different across fronts, the vertical profiles from the same side of a specific front are remarkably uniform from year to year and from cruise to cruise....
Finestructure And Microstructure In The North Atlantic Current, Raymond W. Schmitt, Daniel T. Georgi
Finestructure And Microstructure In The North Atlantic Current, Raymond W. Schmitt, Daniel T. Georgi
Journal of Marine Research
The relationship between intrusive finestructure and optical microstructure was studied by simultaneous CTD Tow-yos and deployments of the shadowgraph profiler SCIMP. Strong thermohaline intrusions, 5 to 50 m thick, were tracked laterally for 5 to 10 km in the front associated with the North Atlantic Current....
Eighteen Degree Water Variability, L. D. Talley, M. E. Raymer
Eighteen Degree Water Variability, L. D. Talley, M. E. Raymer
Journal of Marine Research
The Eighteen Degree Water of the western North Atlantic is formed by deep convection in winter. The circulation and changing properties of Eighteen Degree Water are studied using hydrographic data from a long time series at the Panulirus station (32°10'N, 64°30'W) and from the Gulf Stream '60 experiment....
The Deep Water Of The Central Indian Basin, Bruce A. Warren
The Deep Water Of The Central Indian Basin, Bruce A. Warren
Journal of Marine Research
Two deep CTD sections were occupied by U.S.N.S. Wilkes in the Central Indian Basin during April 1979, one across the basin along Lat. 12S, and the other from Lat. 12S to 1N along Longs. 88-89E. These observations, in combination with other (mostly recent) data, demonstrate a two-layer structure in the deep water of the basin. The upper deep water (2000-3800 m) is supplied from a mid-depth western-boundary current flowing directly northward from the Antarctic along the eastern flank of the Central Indian Ridge....
On The Structure Of The Deep Gulf Stream, R. M. Hendry
On The Structure Of The Deep Gulf Stream, R. M. Hendry
Journal of Marine Research
Tlk zonal and temporal structure of the mean and low-frequency flow beneath the Gulf Stream at 55W is explored in an analysis of 17 months of current and temperature measurements at 4000 m depth….
Variability In The Central Equatorial Indian Ocean Part I: Ocean Dynamics, Michael J. Mcphaden
Variability In The Central Equatorial Indian Ocean Part I: Ocean Dynamics, Michael J. Mcphaden
Journal of Marine Research
Time series of simultaneous wind stress, ocean temperature and velocity from the Island of Gan (00°41'S, 73°10'E) in the equatorial Indian Ocean are examined for the period January 1973-May 1975. Means, trends, and variance at 1 and 2 cycles per year are removed by regression techniques and compared to existing equatorial ocean theories....
Is There A Seasonal Variation In The Agulhas Current?, Alan F. Pearce, Marten L. Gründlingh
Is There A Seasonal Variation In The Agulhas Current?, Alan F. Pearce, Marten L. Gründlingh
Journal of Marine Research
Historical results are critically re-examined for indications of seasonal variability in the surface core speed of the Agulhas Current. Defining the Current core as water flowing southwestward at more than 1 m s-1, it is found that there is no major seasonal variation in mean flow. This is confirmed by more recent direct current measurements.
Variability In The Central Equatorial Indian Ocean, Part Ii: Oceanic Heat And Turbulent Energy Balances, Michael J. Mcphaden
Variability In The Central Equatorial Indian Ocean, Part Ii: Oceanic Heat And Turbulent Energy Balances, Michael J. Mcphaden
Journal of Marine Research
Heat and turbulent energy balances in the central equatorial Indian Ocean are examined using over two years (January 1973-May 1975) of simultaneous oceanic and atmospheric measurements from the island of Gan (00°41S, 73°10'E)….
The Influence Of The Meandering Guiana Current And Amazon River Discharge On Surface Salinity Near Barbados, Gary A. Borstad
The Influence Of The Meandering Guiana Current And Amazon River Discharge On Surface Salinity Near Barbados, Gary A. Borstad
Journal of Marine Research
The seasonal surface salinity regime near Barbados, West Indies is explained in terms of the oceanography of the area. Because of its position relative to the complex and meandering Guiana Current along the northeast coast of South America, the island of Barbados receives mixtures of two fundamentally different surface water types....
Growth And Predation Activity At Deep-Sea Hydrothermal Vents Along The Galápagos Rift, Donald C. Rhoads, Richard A. Lutz, Robert M. Cerrato, Eugene C. Revelas
Growth And Predation Activity At Deep-Sea Hydrothermal Vents Along The Galápagos Rift, Donald C. Rhoads, Richard A. Lutz, Robert M. Cerrato, Eugene C. Revelas
Journal of Marine Research
Growth rates of unclassified mussels collected from hydrothermal vents on the Pacific Ocean (2500 m) are among the highest recorded for deep-sea species. Mature mussels have mean growth rates of about 1 cm yr-1 which are comparable to growth rates of shallow water mussels....
18o Fractionation In Barnacle Calcite: A Barnacle Paleotemperature Equation, J. S. Killingley, W. A. Newman
18o Fractionation In Barnacle Calcite: A Barnacle Paleotemperature Equation, J. S. Killingley, W. A. Newman
Journal of Marine Research
The calcitic shells of sessile barnacles (Balanomorpha) taken from ocean waters ranging in temperature from -2° to 26°C have a near constant 18O enrichment compared with mollusk values assumed to be at thermodynamic equilibrium….
Sources Of Eddy Energy In The Gulf Stream Recirculation Region, Harry L. Bryden
Sources Of Eddy Energy In The Gulf Stream Recirculation Region, Harry L. Bryden
Journal of Marine Research
Array measurements of current and temperature made for 15 months in the main thermodine of the Gulf Stream recirculation region near 31N, 69° 30'W are analyzed to determine the energy sources for low-frequency fluctuations or eddies and the effect of these eddies on the mean circulation in the region....
Oceanic Distribution Of Ammonium-Oxidizing Bacteria Determined By Immunofluorescent Assay, B. B. Ward
Oceanic Distribution Of Ammonium-Oxidizing Bacteria Determined By Immunofluorescent Assay, B. B. Ward
Journal of Marine Research
Marine ammonium-oxidizing bacteria in seawater were enumerated by means of immunofluorescent assays developed for Nitrosococcus oceanus and Nitrosomonas marina. Samples were collected from the coastal waters off the states of Washington and California, from the central North Atlantic and northeast Pacific Oceans, and from Chesapeake Bay....
North Atlantic Circulation And Water Mass Formation, Valentine Worthington
North Atlantic Circulation And Water Mass Formation, Valentine Worthington
Journal of Marine Research
When I returned to Woods Hole after serving in the Navy from 1943 to 1946, I worked as a technician for F. C. Fuglister during his classic descriptions of Gulf Stream meanders and Gulf Stream ring formation. Our work resulted in a joint paper (Fuglister and Worthington, 1951) on a multiple ship survey of the Gulf Stream. It also resulted in my promotion to the scientific staff in September 1951....
Mesopelagic Fishes In Gulf Stream Cold-Core Rings, Richard H. Backus, James E. Craddock
Mesopelagic Fishes In Gulf Stream Cold-Core Rings, Richard H. Backus, James E. Craddock
Journal of Marine Research
Calculations of abundance of midwater fishes in the families Myctophidae, Gonostomatidae, Photichthyidae, and Stemoptychidae for the 1000 m water column were made in cold-core rings and in the nearby Sargasso Sea and Slope Water….
A Note On Sverdrup Balance In The Southern Ocean, D. James Baker Jr.
A Note On Sverdrup Balance In The Southern Ocean, D. James Baker Jr.
Journal of Marine Research
Three sets of recent data from the Southern Ocean, on mass transport through the Drake Passage (Whitworth et al., 1982), on surface winds (Jenne et al., 1971; Han and Lee, 1981) and on density (Gordon et al., 1978) allow an instructive look at the dynamics of the Antarctic Circumpolar Current. These new data suggest that the simple Sverdrup balance of wind stress curl driving a poleward flow south of about 50S as first proposed by Stommel (1957) is consistent with the observed transport within experimental uncertainties....
Observations Of A Barotropic Planetary Wave In The Western North Atlantic, James F. Price, H. Thomas Rossby
Observations Of A Barotropic Planetary Wave In The Western North Atlantic, James F. Price, H. Thomas Rossby
Journal of Marine Research
SOFAR float observations from 1300 m depth are used to describe a major feature of the large-scale, subthermocline velocity field observed in the western North Atlantic (31 N, 70W), during the 1978 POLYMODE Local Dynamics Experiment (LDE). The two-month-long intensive phase of the LDE was dominated by a highly polarized, oscillatory flow which had many of the characteristics of a barotropic planetary wave....
A Theory Of Wind-Driven Circulation. I. Mid-Ocean Gyres, Peter B. Rhines, William R. Young
A Theory Of Wind-Driven Circulation. I. Mid-Ocean Gyres, Peter B. Rhines, William R. Young
Journal of Marine Research
A theory of the wind-driven ocean circulation is presented in which the key feature is strong deformation of interior density layers and consequent production of closed geostrophic-contours by the flow itself. The constraint imposed on the subsurface flow by the imposition of a no flux condition where a geostrophic contour strikes a coastal boundary is thus removed. Within regions where the geostrophic contours close the potential vorticity is uniform....
The Influence Of The Meandering Guiana Current On Surface Conditions Near Barbados - Temporal Variations Of Trichodesmium (Cyanophyta) And Other Plankton, Gary A. Borstad
The Influence Of The Meandering Guiana Current On Surface Conditions Near Barbados - Temporal Variations Of Trichodesmium (Cyanophyta) And Other Plankton, Gary A. Borstad
Journal of Marine Research
The temporal fluctuations of the surface layer Trichodesmium (Cyanophyta) populations off Barbados which occur at roughly three-month intervals are shown to be accompanied by in-phase fluctuations of both the numbers and species composition of other phytoplankton and surface dwelling zooplankton....