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Geophysik II / Geophysics II

  • Book
  • © 1957

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Editors:
  1. Julius Bartels
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Part of the book series: Handbuch der Physik Encyclopedia of Physics (HDBPHYS, volume 10 / 48)

Part of the book sub series: Geophysik / Geophysics (PHYSIK 10)

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Table of contents (17 chapters)

  1. Front Matter

    Pages II-VIII
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  2. Dynamic Meteorology

    • A. Eliassen, E. Kleinschmidt Jr.
    Pages 1-154

  3. Strahlung in der unteren Atmosphäre

    • Fritz Möller
    Pages 155-253

  4. Vision through the Atmosphere

    • W. E. K. Middleton
    Pages 254-287

  5. Polarization of Skylight

    • ZdenÄ›k Sekera
    Pages 288-328

  6. Diffusion des radiations par les gouttes d’eau en suspension dans l’atmosphère

    • J. Bricard
    Pages 329-369

  7. Ozon in der Erdatmosphäre

    • H. K. Paetzold, E. Regener
    Pages 370-426

  8. Geophysical Aspects of Meteors

    • A. C. B. Lovell
    Pages 427-454

  9. Sound Propagation in Air

    • Everett F. Cox
    Pages 455-478

  10. The Physics of Clouds

    • F. H. Ludlam, B. J. Mason
    Pages 479-540

  11. Atmosphärische Elektrizität

    • R. Mühleisen
    Pages 541-607

  12. Oceanography

    • H. U. Sverdrup
    Pages 608-670

  13. Oberflächen-Wellen des Meeres

    • Hans Ulrich Roll
    Pages 671-733

  14. Gezeitenkräfte

    • Julius Bartels
    Pages 734-774

  15. Tides of the Solid Earth

    • Rudolf Tomaschek
    Pages 775-845

  16. Flutwellen und Gezeiten des Wassers

    • A. Defant
    Pages 846-927

  17. Atmosphärische Gezeiten

    • W. Kertz
    Pages 928-981

  18. Physical Volcanology

    • S. Sakuma, T. Nagata
    Pages 982-1011

  19. Back Matter

    Pages 1012-1046
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About this book

45 downwards because (j on the average increases with height; but this conclusion does not follow from (18.3) when the dependency of Kc upon ~o is taken into consideration. s 2 ERTELl and PRIESTLEY and SWINBANK have shown that the upward eddy­ flux of sensible heat must be larger than indicated by (18.3), because this formula does not account for the fact that rising eddies are systematically warmer than sinking eddies because of the effect of buoyancy. The reader is referred to the reviews by SUTTON [22], [23] and PRIESTLEY and SHEP­ PARD [15) for further details concerning eddy-flux of heat and turbulent diffusion. 19. RICHARDSON'S criterion. The right-hand side of (15.10) represents the rate of production of eddy energy. The last term represents energy loss by dissipation; in order that the eddy energy shall be maintained, it is therefore necessary that P div V" - (! V" v" . grad. v > O.

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