Belonenko t v (9 résultats)

Etat : New. pp. 408.

Taschenbuch. Etat : Neu. GRADIENT-VORTICITY WAVES IN THE WORLD OCEAN | General theory. The Southern Ocean. The Pacific Ocean. The Arctic Ocean. | T. V. Belonenko (u. a.) | Taschenbuch | 408 S. | Englisch | 2013 | LAP LAMBERT Academic Publishing | EAN 9783843303491 | Verantwortliche Person für die EU: preigu GmbH & Co. KG, Lengericher Landstr. 19, 49078 Osnabrück, mail[at]preigu[dot]de | Anbieter: preigu.…

Paperback. Etat : Like New. LIKE NEW. SHIPS FROM MULTIPLE LOCATIONS. book.

Taschenbuch. Etat : Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -This book deals with gradient-vorticity oceanic waves, defined as waves whose periods are much longer than the inertial period. The main subject of this book is to study the mechanisms that determine gradient-vorticity wave processes in the ocean. The book consists of an introduction and four parts. The first part deals with the fundamentals of the gradient-vorticity wave theory. Due to the development of satellite altimetry (ERS-1, ERS-2 and TOPEX/POSEIDON), there has been a lot of progress in the work studying low-frequency waves in the ocean. In the last 4 parts of the book the altimetry provides the base of most of the scientific investigation presented from the Southern, Pacific and Arctic Oceans. The description of gradient-vorticity waves begins with the Southern Ocean, where the meridional-boundary effects are small, but planetary and jet effects are most pronounced. In the Pacific, main attention is given to the trapped equatorial waves, Rossby waves, waves in jet streams, and low-frequency waves on the oceanic shelf. The last chapter presents results of studies of trapped low-frequency waves in the Siberian Shelf Seas. 408 pp. Englisch.…

Etat : New. Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. Autor/Autorin: Belonenko T. V.Belonenko Tatyana V., researcher of Saint-Petersburg State University Zakharchuk Evgeny A., head of Saint-Petersburg Branch of State oceanographic institute Foux Victor R., professor of Saint-Petersburg State Univers.…

Taschenbuch. Etat : Neu. nach der Bestellung gedruckt Neuware - Printed after ordering - This book deals with gradient-vorticity oceanic waves, defined as waves whose periods are much longer than the inertial period. The main subject of this book is to study the mechanisms that determine gradient-vorticity wave processes in the ocean. The book consists of an introduction and four parts. The first part deals with the fundamentals of the gradient-vorticity wave theory. Due to the development of satellite altimetry (ERS-1, ERS-2 and TOPEX/POSEIDON), there has been a lot of progress in the work studying low-frequency waves in the ocean. In the last 4 parts of the book the altimetry provides the base of most of the scientific investigation presented from the Southern, Pacific and Arctic Oceans. The description of gradient-vorticity waves begins with the Southern Ocean, where the meridional-boundary effects are small, but planetary and jet effects are most pronounced. In the Pacific, main attention is given to the trapped equatorial waves, Rossby waves, waves in jet streams, and low-frequency waves on the oceanic shelf. The last chapter presents results of studies of trapped low-frequency waves in the Siberian Shelf Seas.…

Taschenbuch. Etat : Neu. This item is printed on demand - Print on Demand Titel. Neuware -This book deals with gradient-vorticity oceanic waves, defined as waves whose periods are much longer than the inertial period. The main subject of this book is to study the mechanisms that determine gradient-vorticity wave processes in the ocean. The book consists of an introduction and four parts. The first part deals with the fundamentals of the gradient-vorticity wave theory. Due to the development of satellite altimetry (ERS-1, ERS-2 and TOPEX/POSEIDON), there has been a lot of progress in the work studying low-frequency waves in the ocean. In the last 4 parts of the book the altimetry provides the base of most of the scientific investigation presented from the Southern, Pacific and Arctic Oceans. The description of gradient-vorticity waves begins with the Southern Ocean, where the meridional-boundary effects are small, but planetary and jet effects are most pronounced. In the Pacific, main attention is given to the trapped equatorial waves, Rossby waves, waves in jet streams, and low-frequency waves on the oceanic shelf. The last chapter presents results of studies of trapped low-frequency waves in the Siberian Shelf Seas.VDM Verlag, Dudweiler Landstraße 99, 66123 Saarbrücken 408 pp. Englisch.…

Etat : New. Print on Demand pp. 408 2:B&W 6 x 9 in or 229 x 152 mm Perfect Bound on Creme w/Gloss Lam.

Etat : New. PRINT ON DEMAND pp. 408.