Koschmieder e l (10 Ergebnisse)

Paperback. Zustand: Good. No Jacket. Pages can have notes/highlighting. Spine may show signs of wear. ~ ThriftBooks: Read More, Spend Less.

Hardcover. Zustand: Good. Zustand des Schutzumschlags: Includes dust jacket. Ex-library copy, with the usual markings/stickers/stamping present. Otherwise cover & text block show minimal shelf & handling wear, crisp and clean. Text/pictures are unmarked, binding intact and firm! A good reading copy.

Zustand: As New. Unread book in perfect condition.

Zustand: Good. First Edition ~1st Printing. Pages intact with minimal writing/highlighting. The binding may be loose and creased. Dust jackets/supplements are not included. Stock photo provided. Product includes identifying sticker. Better World Books: Buy Books. Do Good.

rilegato. Zustand: Perfetto (Mint). Book.

Cloth. Zustand: Very Good. Zustand des Schutzumschlags: Very Good.

Zustand: Gut. 1993, Bibliotheksexemplar - Schutzumschlag: fehlt - Einband: etwas abgerieben, Ecken angestoßen - Seiten: wie ungelesen, leicht nachgedunkelt, Hochglanzpapier.

Zustand: New.

Zustand: New. This book describes the motions resulting from heating a fluid layer from below. Series Editor(s): Ablowitz, Mark J.; Davis, S. H.; Hinch, E. J.; Iserles, A.; Ockendon, J.; Olver, P. J. Series: Cambridge Monographs on Mechanics. Num Pages: 350 pages, 100 b/w illus. BIC Classification: PBT; PBW. Category: (P) Professional & Vocational. Dimension: 228 x 152 x 24. Weight in Grams: 806. . 1993. hardcover. . . . . Books ship from the US and Ireland. …

Buch. Zustand: Neu. Druck auf Anfrage Neuware - Printed after ordering - This book describes the research done on the problems of Bénard convection, as well as its modern offspring the Rayleigh-Bénard problem, and Taylor vortices. Bénard convection differs from Rayleigh-Bénard convection by the presence of surface tension, whilst Bénard convection is characterized by parallel rolls. Toroidal vortices characterize Taylor vortex flow. Convection and Taylor vortex flow deal with the consequences of the presence of infinitesimal disturbances in a fluid layer. Both problems are classical examples in the theory of hydrodynamic stability and share many features. Linear theory describing the onset of instability for both problems is practically completed; nonlinear problems have been at the forefront of research during the last 30 years. The impressive progress that has been made in the theoretical and experimental investigation of the nonlinear problems is described and the remaining basic problems are outlined.…