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Geophysik und Geologie

Geophysik und Geologie PDF Author:
Publisher:
ISBN:
Category : Geology
Languages : de
Pages : 826

Book Description


Geophysik und Geologie

Geophysik und Geologie PDF Author:
Publisher:
ISBN:
Category : Geology
Languages : de
Pages : 826

Book Description


GEOPHYSIK U. GEOLOGIE 4,4

GEOPHYSIK U. GEOLOGIE 4,4 PDF Author:
Publisher:
ISBN: 9783055013799
Category :
Languages : de
Pages :

Book Description


GEOPHYSIK U. GEOLOGIE 4,4

GEOPHYSIK U. GEOLOGIE 4,4 PDF Author: Robert Lauterbach
Publisher:
ISBN: 9783055013799
Category :
Languages : en
Pages : 159

Book Description


Geophysik I / Geophysics I

Geophysik I / Geophysics I PDF Author:
Publisher: Springer Science & Business Media
ISBN: 3642458556
Category : Science
Languages : de
Pages : 667

Book Description


Geophysik und Geologie. Band 3, Heft 4

Geophysik und Geologie. Band 3, Heft 4 PDF Author: R. Lauterbach
Publisher: de Gruyter
ISBN: 9783112525579
Category :
Languages : de
Pages : 0

Book Description


Geophysik II / Geophysics II

Geophysik II / Geophysics II PDF Author:
Publisher: Springer Science & Business Media
ISBN: 3642458815
Category : Science
Languages : de
Pages : 1054

Book Description
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.

Geowissenschaften, Geodäsie, Geophysik, Geologie und Geographie

Geowissenschaften, Geodäsie, Geophysik, Geologie und Geographie PDF Author:
Publisher:
ISBN:
Category :
Languages : de
Pages : 366

Book Description


Geophysik III / Geophysics III

Geophysik III / Geophysics III PDF Author: J. Bartels
Publisher: Springer Science & Business Media
ISBN: 3642460828
Category : Science
Languages : en
Pages : 636

Book Description
7 Fig. 3. Photographie de la lueur nocturne it I'horizon, obtenue it bord d'une fusee Aerobee it 184 km d'altitude Ie ler (l.

Geophysik I / Geophysics I

Geophysik I / Geophysics I PDF Author:
Publisher: Springer
ISBN: 9783540020462
Category : Science
Languages : de
Pages : 660

Book Description


Geophysik III / Geophysics III

Geophysik III / Geophysics III PDF Author: G. Schmidtke
Publisher: Springer Science & Business Media
ISBN: 3642685315
Category : Science
Languages : en
Pages : 552

Book Description
This Encyclopedia aims, basically, at summanzmg the wealth of well established facts and outlining the relevant theories in the different branches of physics. With this as goal, the writers were asked to present their specific field in such a way that access is possible to any scientist without special a priori information in that field; the basic concepts of physics are assumed to be known to the reader. The survey given in each paper was also to be long lasting, so that even a few years after publication, each volume would be useful, for example as an introduction for newcomers or as a source of information for workers in a neighbouring field. In the field of geophysics, dealt with in Vols. 47--49 of the Encyclopedia, this task is difficult to achieve because during the last decades there has been a much faster development of basic information and theory than during the decades before. When I came to contribute to this work the famous Julius Bartels, then editor of the geophysical part, told me that Vol. 49 should certainly take into account the results of the "International Geophysical Year" 1957/58 (I. G. Y. ), and that we had better wait until these were accessible than produce a kind of information which might be obsolete in a short time.