Sprache: Englisch
Verlag: Cambridge University Press., 2008
ISBN 10: 0521055288 ISBN 13: 9780521055284
Anbieter: Universitätsbuchhandlung Herta Hold GmbH, Berlin, Deutschland
Erstausgabe
1st ed. 15 x 23 cm. 368 pages. HC Versand aus Deutschland / We dispatch from Germany via Air Mail. Einband bestoßen, daher Mängelexemplar gestempelt, sonst sehr guter Zustand. Imperfect copy due to slightly bumped cover, apart from this in very good condition. Stamped. Sprache: Englisch.
Sprache: Englisch
Verlag: Cambridge University Press, 2008
ISBN 10: 0521055288 ISBN 13: 9780521055284
Anbieter: Ria Christie Collections, Uxbridge, Vereinigtes Königreich
EUR 73,66
Anzahl: Mehr als 20 verfügbar
In den WarenkorbZustand: New. In.
Sprache: Englisch
Verlag: Cambridge University Press, 2008
ISBN 10: 0521055288 ISBN 13: 9780521055284
Anbieter: Kennys Bookstore, Olney, MD, USA
EUR 105,18
Anzahl: Mehr als 20 verfügbar
In den WarenkorbZustand: New. The work explores the potential for inverse theory which can combine observations of ocean circulation with numerical models. Series: Cambridge Monographs on Mechanics. Num Pages: 368 pages, 102 b/w illus. 9 tables. BIC Classification: PBW; RBKC. Category: (P) Professional & Vocational; (U) Tertiary Education (US: College). Dimension: 229 x 156 x 23. Weight in Grams: 586. . 2008. 1st Edition. paperback. . . . . Books ship from the US and Ireland.
Sprache: Englisch
Verlag: Cambridge University Press, 2008
ISBN 10: 0521055288 ISBN 13: 9780521055284
Anbieter: AHA-BUCH GmbH, Einbeck, Deutschland
Taschenbuch. Zustand: Neu. Druck auf Anfrage Neuware - Printed after ordering - Observations of ocean circulation have increased as a result of international field programmes and of remote sensing systems on artificial earth satellites. Oceanographers are increasingly turning to inverse methods for combining these observations with numerical models of ocean circulation. Professor Bennett's work explores the potential for inverse theory, emphasizing possibilities rather than expedient or rudimentary applications. In addition to interpolating the data and adding realism to the model solutions, the methods can yield estimates for unobserved flow variables, forcing fields, and model parameters. Inverse formulations can resolve ill-posed modelling problems, lead to design criteria for oceanic observing systems, and enable the testing of models as scientific hypothesis. Exercises of varying difficulty rehearse technical skills and supplement the central theoretical development. Thus this book will be invaluable for environmental scientists and engineers, advanced undergraduates in applied mathematics, and graduate students in physical oceanography.