Geophysik II Geophysics II SpringerLink

Geophysik II Geophysics II SpringerLink

Geophysik II / Geophysics II SpringerLink Skip to main content Advertisement Search Go to cart Search Book © 1957

Geophysik II Geophysics II

Editors

Julius Bartels Julius Bartels View editor publications You can also search for this editor in PubMed Google Scholar 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) 7955 Accesses 153 Citations

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Table of contents About this book Keywords Bibliographic Information

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Table of contents 17 chapters

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Front Matter

Pages II-VIII PDF

Dynamic Meteorology

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

Strahlung in der unteren Atmosphäre

Fritz Möller Pages 155-253

Vision through the Atmosphere

W. E. K. Middleton Pages 254-287

Polarization of Skylight

Zdeněk Sekera Pages 288-328

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

J. Bricard Pages 329-369

Ozon in der Erdatmosphäre

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

Geophysical Aspects of Meteors

A. C. B. Lovell Pages 427-454

Sound Propagation in Air

Everett F. Cox Pages 455-478

The Physics of Clouds

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

Atmosphärische Elektrizität

R. Mühleisen Pages 541-607

Oceanography

H. U. Sverdrup Pages 608-670

Oberflächen-Wellen des Meeres

Hans Ulrich Roll Pages 671-733

Gezeitenkräfte

Julius Bartels Pages 734-774

Tides of the Solid Earth

Rudolf Tomaschek Pages 775-845

Flutwellen und Gezeiten des Wassers

A. Defant Pages 846-927

Atmosphärische Gezeiten

W. Kertz Pages 928-981

Physical Volcanology

S. Sakuma, T. Nagata Pages 982-1011

Back Matter

Pages 1012-1046 PDF Back to top

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. Back to top

Keywords

Wellenatmospheredensitydiffractiondiffusiondynamicselectricityenergygeophysicsgravitationheathydrodynamicsphysicsradiationwave Back to top

Bibliographic Information

Book Title: Geophysik II Geophysics II Editors Julius Bartels Series Title: Handbuch der Physik Encyclopedia of Physics DOI: https://doi.org/10.1007/978-3-642-45881-1 Publisher: Springer Berlin, Heidelberg eBook Packages: Springer Book Archive Copyright Information: Springer-Verlag Berlin Heidelberg 1957 Softcover ISBN: 978-3-642-45883-5 eBook ISBN: 978-3-642-45881-1 Series ISSN: 0085-140X Series E-ISSN: 2197-4195 Edition Number: 1 Number of Pages: VIII, 1046 Topics: Geophysics, Environmental Physics, Physics and Astronomy Back to top Access via your institution

Buying options

eBook USD 169.00 Price excludes VAT (USA) ISBN: 978-3-642-45881-1 Instant PDF download Readable on all devices Own it forever Exclusive offer for individuals only Tax calculation will be finalised during checkout Buy eBook Softcover Book USD 219.99 Price excludes VAT (USA) ISBN: 978-3-642-45883-5 Dispatched in 3 to 5 business days Exclusive offer for individuals only Free shipping worldwide
Shipping restrictions may apply, check to see if you are impacted. Tax calculation will be finalised during checkout Buy Softcover Book Learn about institutional subscriptions
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