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  • 1
    Monograph available for loan
    Monograph available for loan
    Massachusetts : Woods Hole Oceanographic Institution
    Associated volumes
    Call number: PIK N 454-97-0256
    In: On the world ocean circulation
    Type of Medium: Monograph available for loan
    Pages: IV, 237 S.
    Series Statement: On the world ocean circulation
    Location: A 18 - must be ordered
    Branch Library: PIK Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    Massachusetts : Woods Hole Oceanographic Institution
    Associated volumes
    Call number: PIK N 454-97-0255
    In: On the world ocean circulation
    Type of Medium: Monograph available for loan
    Pages: IV, 141 S.
    Series Statement: On the world ocean circulation
    Branch Library: PIK Library
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  • 3
    Publication Date: 2022-05-25
    Description: This is the first volume of a "final report" that summarizes, often in a speculative vein, what I have learned over the past 35 years or so about large-scale, low-frequency ocean currents, primarily with support from the Office of Naval Research (ONR). I was also fortunate to have been partially supported by the National Science Foundation and, during the preparation of this report, by the Clark Foundation. This report is meant to be an informal, occasionally anecdotal, state-of-the-art summary account of the World Ocean Circulation (WOC). Seemingly simple questions about how ocean currents behave, such as where various brands of sea water are coming from and going to, have been exciting and difficult research topics for many years. This report is not remotely about "all" of the WOC, it is simply a set of comments about what I have looked into. I believe that the results in this report, although presented in a personal way, are consistent with community wisdom. The report is intended to be readable by non-specialists who have a basic scientific/technical background, especially in other oceanographic areas or meteorology or physics or the geophysical disciplines, not just by specialists in physical oceanography. Anyone wishing to get spun up on the observational basis for the WOC could use this report and associated reference lists as a starting point. Volume I concentrates on the North Atlantic Ocean although there is preliminary discussion of global features. Highlights of this global summary are a new type of composite schematic picture of the World Ocean Circulation in its "upper layers" (Figure I-I) and new summaries (Figures 1-12, 21,91) of the global "thermohaline" circulation.
    Description: Funding was provided by the Office of Naval Research, Grant Nos. N00014-89-J-1039 and N00014-95-1-0356, and the Clark Foundation.
    Keywords: Global ocean circulation ; North Atlantic Circulation ; Ocean currents
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
    Format: 39418867 bytes
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  • 4
    Publication Date: 2022-05-25
    Description: Neutrally buoyant SOFAR floats at nominal depths of 800 m, 1800 m, and 3300 m were tracked acoustically for 3.7 years in the vicinity of the western boundary and the equator of the Atlantic Ocean. Trajectories and summaries from the whole experiment are shown along with detailed trajectories from the second setting of the listening stations, October 1990 to September 1992. Some highlights are mentioned below. Trajectories at 1800 m revealed a swift narrow southward flowing deep western boundary current (DWBC) extending from 7°N across the equator. Two floats directly crossed the equator in the DWBC and went to 10°S. Two other floats left the DWBC near the equator and drifted eastward. Three floats entered the DWBC from the equatorial current system and drifted southward. No obvious DWBC or swift equatorial currents were observed by the 3300 m floats. The 800 m floats plus some surface drifters measured seven anticyclonic eddies as they translated northwestward along the coast of South America in a band from the equator to 12°N. One of the floats (28) entered the Caribbean where tracking stopped. This float was again tracked as it drifted across the mid-Atlantic Ridge and entered the Canary Basin near 34°N 28°W after a gap of 2.7 years. We infer that this float went westward though the Caribbean and northeastward in the Gulf Stream. Float 17 drifted northward from 10°N to 22°N in an eastern boundary current off the coast of West Africa. Floats between 6°N-6°S (roughly) drifted long distances zonally in the equatorial current system.
    Description: Funding was provided by the National Science Foundation through Grants Nos. OCE85-21082, OCE85-17375, and OCE91-14656.
    Keywords: SOFAR floats ; Sound Fixing And Ranging floats ; Equatorial currents
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 5
    Publication Date: 2022-05-25
    Description: Author Posting. © American Meteorological Society, 2015. This article is posted here by permission of American Meteorological Society for personal use, not for redistribution. The definitive version was published in Journal of Physical Oceanography 45 (2015): 2913–2932, doi:10.1175/JPO-D-14-0179.1.
    Description: The oceanic deep circulation is shared between concentrated deep western boundary currents (DWBCs) and broader interior pathways, a process that is sensitive to seafloor topography. This study investigates the spreading and deepening of Denmark Strait overflow water (DSOW) in the western subpolar North Atlantic using two ° eddy-resolving Atlantic simulations, including a passive tracer injected into the DSOW. The deepest layers of DSOW transit from a narrow DWBC in the southern Irminger Sea into widespread westward flow across the central Labrador Sea, which remerges along the Labrador coast. This abyssal circulation, in contrast to the upper levels of overflow water that remain as a boundary current, blankets the deep Labrador Sea with DSOW. Farther downstream after being steered around the abrupt topography of Orphan Knoll, DSOW again leaves the boundary, forming cyclonic recirculation cells in the deep Newfoundland basin. The deep recirculation, mostly driven by the meandering pathway of the upper North Atlantic Current, leads to accumulation of tracer offshore of Orphan Knoll, precisely where a local maximum of chlorofluorocarbon (CFC) inventory is observed. At Flemish Cap, eddy fluxes carry ~20% of the tracer transport from the boundary current into the interior. Potential vorticity is conserved as the flow of DSOW broadens at the transition from steep to less steep continental rise into the Labrador Sea, while around the abrupt topography of Orphan Knoll, potential vorticity is not conserved and the DSOW deepens significantly.
    Description: This work is supported by ONR Award N00014-09-1-0587, the NSF Physical Oceanography Program, and NASA Ocean Surface Topography Science Team Program.
    Description: 2016-06-01
    Keywords: Circulation/ Dynamics ; Abyssal circulation ; Boundary currents ; Ocean circulation ; Ocean dynamics ; Potential vorticity ; Topographic effects
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 6
    Publication Date: 2022-05-26
    Description: Neutrally buoyant SOFAR floats at nominal depths of 800, 1800, and 3300 m were tracked for 21 months in the vicinity of western boundary currents near 6N and at several sites in the Atlantic near 11N and along the equator. Trajectories at 1800 m show a swift (〉50 cm/sec), narrow (100 km wide) southward-flowing Deep Western Boundary Current (DWBC) extending from 7N to the equator. At times (February-March 1989) DWBC water turned eastward and flowed along the equator and at other times (August-September 1990) the DWBC crossed the equator and continued southward. The mean velocity near the equator was eastward from February 1989 to February 1990 and westward from March 1990 to November 1990. Thus the cross-equatorial flow in the DWBC appeared to be linked to the direction of equatorial currents which varied over periods of more than a year. No obvious DWBC nor swift equatorial current was observed by 3300 m floats. Eight-hundred-meter floats revealed a northwestward intermediate level western boundary current although flow patterns were complicated. Three floats that significantly contributed to the northwestward flow looped in anticyclonic eddies that translated up the coast at 8 cm/sec. Six 800 m floats drifted eastward along the equator between 5S and 6N at a mean velocity of 11 cm/sec; one reached 5W in the Gulf of Guinea, suggesting that the equatorial current extended at least 35-40° along the equator. Three of these floats reversed direction near the end of the tracking period, implying low frequency fluctuations.
    Description: Funding was provided by the National Science Foundation through Grant Nos. OCE-8521082, OCE-8517375, and OCE-9114656.
    Keywords: SOFAR floats ; Equatorial currents ; Deep Western Boundary Current ; Oceanus (Ship : 1975-) Cruise ; Columbus Iselin (Ship) Cruise
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 7
    Publication Date: 2022-05-26
    Description: This is the second and final volume of a report that describes some of my investigations over the last 35 years or so into low-frequency ocean current structures, a topic which I will call the World Ocean Circulation (WOC). The material presented constitutes my final report to the Office of Naval Research, and their support over the years is deeply appreciated. I was also fortunate to have been partially supported by the National Science Foundation during my career and, for some of the preparation of this report, by the Clark Foundation. Volume I was focused on the North Atlantic Ocean, after a global scale summary. This volume (II) will consider first the Pacific and Indian Oceans, concentrating on interbasin circulations, meridional cells, and mesoscale eddy fields. Then, there is an exceptionaly brief discussion of the Southern Ocean(s) for background only, followed by a global summary. Lately, I have worked intensely on intergyre and interbasin exchanges, including an inter-comparison of some of the properties of the eddy field in the World's Oceans (Schmitz, W.J., Jr., Reo. Geophys.,33,151-173,1995; J. Geophys. Res., 101,16,259-16,271,1996). Volume II contains not only an update of the global picture, but also new representations of the transport structure of various components of the meridional overturning cells for each ocean. In summary, several similarties as well as dissimilarities between different oceans relative to both their general circulation and their mesoscale eddy field are shown to be associated with interbasin exchanges. This report is meant to be an informal, occasionaly anecdotal, state-of-the-art summary account of the World Ocean Circulation. Seemingly simple questions about how ocean currents behave, such as where various brands of sea water are coming from and going to, have been exciting research topics for many years. This report is not remotely about "all" of the WOC, it is simply a set of comments about what I have looked into during the preparation of this document. I do believe that the results in this report, although presented in a personal way, are consistent with community wisdom. The document is intended to be readable by non-specialists who have a basic scientifc/technical background, especially in other oceanographic areas or meteorology or the geophysical disciplines, not only by specialists in physical oceanography.
    Description: Funding was provided by the Office of Naval Research, Grant Nos. NO0014-89-J-I039 and N00014-95-1-0356, and the Clark Foundation.
    Keywords: Global ocean circulation ; Ocean currents
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 8
    Publication Date: 2022-05-26
    Description: Also published as: Journal. of Marine Research 38 (1980): 215-248
    Description: As a sequel to Schmitz and Hogg (1978), nine-month moored observations of current and temperature from the Charlie Gibbs Fracture Zone are further described, and then interpreted in terms of low frequency quasigeostrophic motions. Large vertical and horizontal changes are observed in the variance of both mean and fluctuating components. It is demonstrated that these changes could be associated with the (complex) nature of the topography. With regard to the mean flow, it is shown through an advective model that the topography is sufficiently steep to force this motion to closely follow isobaths. Time-dependent motions for periods from 2 to 96 days are described using the technique of empirical orthogonal functions. The most energetic mode is always bottom trapped, with flow oriented along isobaths at lower frequencies and approaching equipartition of along- and cross-isobath motions at higher frequencies. At the lowest frequencies a second mode which increases upward in energy is also judged significant, while for periods shorter than 3.6 days the second mode is again highly bottom trapped. We interpret these motions using linear wave theory. There is relatively close correspondence between theory and observation when the effects of both large- and small-scale topographic features are included in the model calculations. In addition to the usual topographic wave, the abrupt slope changes on the north wall allow for a baroclinic fringe mode with a ncar bottom node at low frequencies and small-scale bottom corrugations force highly bottom trapped waves above the smooth slope cut-off frequency.
    Description: Prepared for the Office of Naval. Research under Contract N00014-76-C-0197; NR 083- 400.
    Keywords: Ocean bottom ; Submarine topography ; Charles Gibbs Fracture Zone
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 9
    Publication Date: 2022-05-26
    Description: Also published as: Journal of Marine Research 36 (1978): 725-734
    Description: Relatively energetic low frequency fluctuations in horizontal currents are found to exist below the thermocline in the northern trough of the Charlie-Gibbs Fracture Zone. For example, deep eddy kinetic energy levels there are about twice as large as those observed at similar relative depths in the MODE-I region. Eddy kinetic energies are about 2-10 times larger than mean kinetic energies. The vertical distribution of eddy kinetic energy is frequency dependent, increasing toward the thermocline for the longer time scales and intensifying toward the bottom at higher frequencies. In addition to the expected mean westward motion of Norwegian Sea Overflow Water through the northern trough of the fracture, rather consistent mean southward flow is observed at a depth immediately above the overflow.
    Description: Prepared f or the Office of Naval Research under Contract N00014-76-C-0197; NR 083- 400.
    Keywords: Ocean circulation ; Ocean currents ; Charles Gibbs Fracture Zone
    Repository Name: Woods Hole Open Access Server
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  • 10
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    Woods Hole Oceanographic Institution
    Publication Date: 2022-05-26
    Description: Also published as: Journal of Marine Research, Volume 35, 1977, pp. 21-28
    Description: Very large (5-10 cm s-1) long-term averaged zonal flows have been observed near 4000 m depth in the vicinity of a recently hypothesized (Worthington, in press) horizontally restricted subtropical gyre in the deep western North Atlantic. The Reynolds stresses associated with low frequency fluctuations may play a significant role in the dynamics of this deep mean flow, possibly inducing a significant downstream increase in transport of the Gulf Stream, perhaps driving the deep gyre.
    Description: Prepared for the Office of Naval Research under Contracts N00014-66-C-0241; NR 083- 004 and N00014-74-C-0262; NR 083-004 and for the International Decade of Ocean Exploration of the National Science Foundation under Grant OCE75-03962.
    Keywords: Ocean circulation
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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