ISBN: 9780387964454 - the physical nature and structure of oceanic fronts (coastal and estuarine studies, 19, band 19) (12 Ergebnisse)

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  • Sprache: Englisch

    Verlag: Springer (edition Softcover reprint of the original 1st ed. 1986), 1986

    0387964452 / 9780387964454

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    Paperback. Zustand: Very Good. It's a well-cared-for item that has seen limited use. The item may show minor signs of wear. All the text is legible, with all pages included. It may have slight markings and/or highlighting. Softcover reprint of the original 1st ed. 1986.

  • Sprache: Englisch

    Verlag: Springer, 1986

    0387964452 / 9780387964454

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  • Sprache: Englisch

    Verlag: Springer, 1986

    0387964452 / 9780387964454

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  • Sprache: Englisch

    Verlag: Springer, 1986

    0387964452 / 9780387964454

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    Zustand: New. pp. 344.

  • Sprache: Englisch

    Verlag: Springer Verlag, 1986

    0387964452 / 9780387964454

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    Paperback. Zustand: Brand New. 1st edition. 341 pages. 9.61x6.69x0.78 inches. In Stock.

  • Sprache: Englisch

    Verlag: Springer, 1986

    0387964452 / 9780387964454

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    Taschenbuch. Zustand: Neu. Druck auf Anfrage Neuware - Printed after ordering - During the past several years, research into the frontal divisions of the ocean has been particularly intensive. The significance of this lies not only in the fact that, in the five years from 1976 to 1980, more than 500 papers on this question were published in various journals throughout the world and at least three major international discussions were held (see p. 17). The newness of the discussion of the topic stems from the qualitative reinterpretation of the physical essence of the phenomenon and its role in the ocean, particularly in the processes of mixing and structure formation. While in the past the conventional view of fronts as boundaries between large scale water masses of the ocean only led to the recognition of convenient classi fication limits created by nature itself, there is now a tendency to study oceanic fronts as integral elements of the dynamics of oceanic waters. As we understand it, fronts are being associated more and more with the dynamic and kinematic features which arise when kinetic energy and enstrophy are transmitted through a cascade of scales characterizing various forms of motion of a stratified medium in laterally confined oceanic basins. We are beginning to get a better understanding of the role synoptic-scale oceanic eddies play in the process of frontogenesis in the ocean.…

  • Sprache: Englisch

    Verlag: Springer 1986-12, 1986

    0387964452 / 9780387964454

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    PF. Zustand: New. This item is printed on demand. Brand new book, sourced directly from publisher. Dispatch time is 6-7 days from our warehouse. Book will be sent in robust, secure packaging to ensure it reaches you securely.

  • Sprache: Englisch

    Verlag: Springer New York, Springer Dez 1986, 1986

    0387964452 / 9780387964454

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    Taschenbuch. Zustand: Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -During the past several years, research into the frontal divisions of the ocean has been particularly intensive. The significance of this lies not only in the fact that, in the five years from 1976 to 1980, more than 500 papers on this question were published in various journals throughout the world and at least three major international discussions were held (see p. 17). The newness of the discussion of the topic stems from the qualitative reinterpretation of the physical essence of the phenomenon and its role in the ocean, particularly in the processes of mixing and structure formation. While in the past the conventional view of fronts as boundaries between large scale water masses of the ocean only led to the recognition of convenient classi fication limits created by nature itself, there is now a tendency to study oceanic fronts as integral elements of the dynamics of oceanic waters. As we understand it, fronts are being associated more and more with the dynamic and kinematic features which arise when kinetic energy and enstrophy are transmitted through a cascade of scales characterizing various forms of motion of a stratified medium in laterally confined oceanic basins. We are beginning to get a better understanding of the role synoptic-scale oceanic eddies play in the process of frontogenesis in the ocean. 344 pp. Englisch.…

  • Sprache: Englisch

    Verlag: Springer, 1986

    0387964452 / 9780387964454

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    Zustand: New. Print on Demand pp. 344 67:B&W 6.69 x 9.61 in or 244 x 170 mm (Pinched Crown) Perfect Bound on White w/Gloss Lam.

  • Sprache: Englisch

    Verlag: Springer New York, 1986

    0387964452 / 9780387964454

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    Zustand: New. Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. During the past several years, research into the frontal divisions of the ocean has been particularly intensive. The significance of this lies not only in the fact that, in the five years from 1976 to 1980, more than 500 papers on this question were publish.…

  • Sprache: Englisch

    Verlag: Springer, 1986

    0387964452 / 9780387964454

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    Zustand: New. PRINT ON DEMAND pp. 344.

  • Sprache: Englisch

    Verlag: Springer, Springer Dez 1986, 1986

    0387964452 / 9780387964454

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    Taschenbuch. Zustand: Neu. This item is printed on demand - Print on Demand Titel. Neuware -During the past several years, research into the frontal divisions of the ocean has been particularly intensive. The significance of this lies not only in the fact that, in the five years from 1976 to 1980, more than 500 papers on this question were published in various journals throughout the world and at least three major international discussions were held (see p. 17). The newness of the discussion of the topic stems from the qualitative reinterpretation of the physical essence of the phenomenon and its role in the ocean, particularly in the processes of mixing and structure formation. While in the past the conventional view of fronts as boundaries between large scale water masses of the ocean only led to the recognition of convenient classi fication limits created by nature itself, there is now a tendency to study oceanic fronts as integral elements of the dynamics of oceanic waters. As we understand it, fronts are being associated more and more with the dynamic and kinematic features which arise when kinetic energy and enstrophy are transmitted through a cascade of scales characterizing various forms of motion of a stratified medium in laterally confined oceanic basins. We are beginning to get a better understanding of the role synoptic-scale oceanic eddies play in the process of frontogenesis in the ocean.Springer-Verlag KG, Sachsenplatz 4-6, 1201 Wien 344 pp. Englisch. …