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  • 1
    Online Resource
    Online Resource
    Berlin, Heidelberg :Springer Berlin / Heidelberg,
    Keywords: Ocean circulation. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (463 pages)
    Edition: 1st ed.
    ISBN: 9783662032046
    DDC: 551.47
    Language: English
    Note: Ocean Circulation Theory -- Copyright -- Preface -- Contents -- 1 Sverdrup Theory -- 2 Homogeneous Models of the Ocean Circulation -- 3 Vertical Structure: Baroclinic Quasi-Geostrophic Models -- 4 Theory of the Ventilated Thermocline -- 5 Buoyancy Forced Circulation and Cross-Gyre Flow -- 6 Equatorial Dynamics of the Thermocline: The Equatorial Undercurrent -- 7 Abyssal Circulation -- Subject Index.
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  • 2
    Book
    Book
    New York, N.Y. : Springer
    Type of Medium: Book
    Pages: XII, 624 S , graph. Darst
    Edition: 2. printing
    ISBN: 0387907459 , 3540907459 , 0387903682 , 3540903682
    Series Statement: Springer study edition
    Language: Undetermined
    Note: Based on corrected 2. print. of orig. ed , Literaturverz. S. 605 - 617
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  • 3
    Book
    Book
    New York : Springer
    Keywords: Fluid dynamics ; Geophysics ; Geophysik ; Hydrodynamik ; Strömungsmechanik ; Atmosphäre
    Description / Table of Contents: Ohne Kurzreferat
    Type of Medium: Book
    Pages: XIV, 710 S , graph. Darst , 25 cm
    Edition: 2. ed
    ISBN: 3540963871 , 0387963871 , 354096388X , 038796388X
    Series Statement: Springer study edition
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    Language: English
    Note: Literaturverz. S. [689] - 703
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  • 4
    Book
    Book
    Venice : Consiglio Nazionale delle Ricerche, Ist. Biologia del Mare [u.a.]
    Keywords: Meeresströmung
    Type of Medium: Book
    Pages: 124 S , graph. Darst , 24 cm
    Series Statement: Environmental dynamics series 1
    DDC: 551.47
    Language: English
    Note: Includes bibliographical references (p. 87-89)
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  • 5
    Book
    Book
    Berlin : Springer
    Keywords: Ocean circulation ; Meereskunde ; Zirkulation ; Mathematisches Modell
    Type of Medium: Book
    Pages: XI, 453 S. , graph. Darst., Kt.
    ISBN: 0387604898 , 3540604898
    DDC: 551.47
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    Language: English
    Note: Literaturangaben
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  • 6
    Keywords: Ocean waves ; Atmospheric waves ; Atmosphäre ; Gleichung ; Kinematik ; Laplace Gleichung ; Luft ; Modell ; Ozeane ; Physik ; Rossby waves ; Wellen ; Meereswelle ; Hydrodynamik ; Atmosphäre ; Wellenbewegung ; Atmosphäre ; Wellenausbreitung ; Meer ; Wellenausbreitung
    Description / Table of Contents: The text presents a treatment of the fundamental theory of waves. Starting with an elementary treatment of the basic wave concept, specific wave phenomena are treated including: surface gravity waves, internal gravity waves, lee waves, waves in the presence of rotation, geostrophic adjustment, quasi-geostrophic waves and potential vorticity, wave-mean flow interaction, unstable waves. Each wave topic is used to introduce either a new technique or concept in general wave theory. The book contains numerous end-of-chapter exercises. (MOD)
    Type of Medium: Book
    Pages: VIII, 260 S , graph. Darst , 25 cm
    ISBN: 3540003401
    DDC: 551.4702
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    Language: English
    Note: Literaturverz. S. [249] - 251
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  • 7
    Book
    Book
    New York : Springer
    Type of Medium: Book
    Pages: XII, 624 S. , graph. Darst.
    ISBN: 0387903682 , 3540903682 , 0387907459 , 3540907459
    DDC: 551
    RVK:
    RVK:
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    Language: English
    Note: Literaturverz. S. 605 - 617
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  • 8
    Publication Date: 2022-05-25
    Description: Author Posting. © American Meteorological Society, 2010. 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 40 (2010): 1075-1086, doi:10.1175/2009JPO4375.1.
    Description: A quasigeostrophic, two-layer model is used to study the baroclinic circulation around a thin, meridionally elongated island. The flow is driven by either buoyancy forcing or wind stress, each of whose structure would produce an antisymmetric double-gyre flow. The ocean bottom is flat. When the island partially straddles the intergyre boundary, fluid from one gyre is forced to flow into the other. The amount of the intergyre flow depends on the island constant, that is, the value of the geostrophic streamfunction on the island in each layer. That constant is calculated in a manner similar to earlier studies and is determined by the average, along the meridional length of the island, of the interior Sverdrup solution just to the east of the island. Explicit solutions are given for both buoyancy and wind-driven flows. The presence of an island of nonzero width requires the determination of the baroclinic streamfunction on the basin’s eastern boundary. The value of the boundary term is proportional to the island’s area. This adds a generally small additional baroclinic intergyre flow. In all cases, the intergyre flow produced by the island is not related to topographic steering of the flow but rather the pressure anomaly on the island as manifested by the barotropic and baroclinic island constants. The vertical structure of the flow around the island is a function of the parameterization of the vertical mixing in the problem and, in particular, the degree to which long baroclinic Rossby waves can traverse the basin before becoming thermally damped.
    Description: This research was supported in part by NSF Grant OCE 0451086.
    Keywords: Gyres ; Baroclinic flows ; Topographic effects ; Streamfunction ; Orographic effects
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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  • 9
    Publication Date: 2022-05-25
    Description: Author Posting. © American Meteorological Society, 2009. 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 39 (2009): 1541-1550, doi:10.1175/2008JPO3999.1.
    Description: The response of a zonal channel to a uniform, switched-on but subsequently steady poleward outflow is presented. An eastward coastal current with a Kelvin wave’s cross-shore structure is found to be generated instantly upon initiation of the outflow. The current is essentially in geostrophic balance everywhere except for the vicinity of the outflow channel mouth, where the streamlines must cross planetary vorticity contours to feed the current. The adjustment of this region generates a plume that propagates westward at Rossby wave speeds. The cross-shore structure of the plume varies with longitude, and at any given longitude it evolves with time. The authors show that the plume evolution can be understood both conceptually and quantitatively as the westward propagation of the Kelvin current’s meridional spectrum, with each spectral element propagating at its own Rossby wave group velocity.
    Description: This work was completed at Woods Hole Oceanographic Institution while T.S. Durland was supported by the Ocean and Climate Change Institute. M.A. Spall was supported by NSF Grant OCE-0423975, and J. Pedlosky by NSF Grant OCE-0451086. T.S. Durland acknowledges additional report preparation support from NASA Grant NNG05GN98G.
    Keywords: Coastal flows ; Estuaries ; Currents ; Vorticity ; Plumes
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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  • 10
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    American Meteorological Society
    Publication Date: 2022-05-25
    Description: Author Posting. © American Meteorological Society, 2008. 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 38 (2008): 1267-1277, doi:10.1175/2007JPO3906.1.
    Description: A two-layer quasigeostrophic model in a channel is used to study the influence of lateral displacements of regions of different sign mean potential vorticity gradient (Πy) on the growth rate and structure of linearly unstable waves. The mean state is very idealized, with a region of positive Πy in the upper layer and a region of negative Πy in the lower layer; elsewhere Πy is zero. The growth rate and structure of the model’s unstable waves are quite sensitive to the amount of overlap between the two regions. For large amounts of overlap (more than several internal deformation radii), the channel modes described by Phillips’ model are recovered. The growth rate decreases abruptly as the amount of overlap decreases below the internal deformation radius. However, unstable modes are also found for cases in which the two nonzero Πy regions are separated far apart. In these cases, the wavenumber of the unstable waves decreases such that the aspect ratio of the wave remains O(1). The waves are characterized by a large-scale barotropic component that has maximum amplitude near one boundary but extends all the way across the channel to the opposite boundary. Near the boundaries, the wave is of mixed barotropic–baroclinic structure with cross-front scales on the order of the internal deformation radius. The perturbation heat flux is concentrated near the nonzero Πy regions, but the perturbation momentum flux extends all the way across the channel. The perturbation fluxes act to reduce the isopycnal slopes near the channel boundaries and to transmit zonal momentum from the region of Πy 〉 0 to the region on the opposite side of the channel where Πy 〈 0. These nonzero perturbation momentum fluxes are found even for a mean state that has no lateral shear in the velocity field.
    Description: This work was supported by NSF Grants OPP-0421904, OCE-0423975 (MAS), and OCE- 85108600 (JP).
    Keywords: Baroclinic flows ; Barotropic flows
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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