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Baroclinic tides : theoretical modeling and observational evidence /
When an oceanic tidal wave that is primarily active on the water surface passes an ocean shelf or a region with a seamount, it is split into a less energetic surface wave and other internal modes with different wavelengths and propagation speeds. This cascading process, from the barotropic tides to...
| Clasificación: | Libro Electrónico |
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| Autor principal: | |
| Otros Autores: | , |
| Formato: | Electrónico eBook |
| Idioma: | Inglés |
| Publicado: |
New York :
Cambridge University Press,
2005.
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| Temas: | |
| Acceso en línea: | Texto completo |
MARC
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| 049 | |a UAMI | ||
| 100 | 1 | |a Vlasenko, Vasiliy. | |
| 245 | 1 | 0 | |a Baroclinic tides : |b theoretical modeling and observational evidence / |c Vasiliy Vlasenko, Nataliya Stashchuk, Kolumban Hutter. |
| 260 | |a New York : |b Cambridge University Press, |c 2005. | ||
| 300 | |a 1 online resource (1 volume) | ||
| 336 | |a text |b txt |2 rdacontent | ||
| 337 | |a computer |b c |2 rdamedia | ||
| 338 | |a online resource |b cr |2 rdacarrier | ||
| 504 | |a Includes bibliographical references and index. | ||
| 588 | 0 | |a Print version record. | |
| 520 | |a When an oceanic tidal wave that is primarily active on the water surface passes an ocean shelf or a region with a seamount, it is split into a less energetic surface wave and other internal modes with different wavelengths and propagation speeds. This cascading process, from the barotropic tides to the baroclinic components, leads to the transformation of tidal energy into turbulence and heat, an important process for the dynamics of the lower ocean. Baroclinic Tides demonstrates the analytical and numerical methods used to study the generation and evolution of baroclinic tides and, by comparison with experiments and observational data, shows how to distinguish and interpret internal waves. Strongly non-linear solitary internal waves, which are generated by internal tidal waves at the final stage of their evolution, are investigated in detail. This book is intended for researchers and graduate students of physical oceanography, geophysical fluid dynamics and hydroacoustics. | ||
| 505 | 0 | |a Cover; Half-title; Title; Copyright; Dedication; Contents; Tables; Preface; Acknowledgements; Symbols; Abbreviations; Preamble; 1 General background; 2 Linear baroclinic tides over variable bottom topography; 3 Combined effect of horizontal density gradient and bottom topography on the dynamics of linear baroclinic tides; 4 Topographic generation of nonlinear baroclinic tides; 5 Evolutionary stages of baroclinic tides; 6 Generation mechanism for different background conditions; 7 Three-dimensional effects of baroclinic tides; References; Index | |
| 590 | |a eBooks on EBSCOhost |b EBSCO eBook Subscription Academic Collection - Worldwide | ||
| 650 | 0 | |a Baroclinic models. | |
| 650 | 0 | |a Baroclinicity. | |
| 650 | 0 | |a Dynamic meteorology |x Mathematical models. | |
| 650 | 6 | |a Modèles baroclines. | |
| 650 | 6 | |a Instabilité barocline. | |
| 650 | 6 | |a Météorologie dynamique |x Modèles mathématiques. | |
| 650 | 7 | |a SCIENCE |x Earth Sciences |x Oceanography. |2 bisacsh | |
| 650 | 7 | |a NATURE |x Ecosystems & Habitats |x Oceans & Seas. |2 bisacsh | |
| 650 | 7 | |a Baroclinic models. |2 fast |0 (OCoLC)fst00827693 | |
| 650 | 7 | |a Baroclinicity. |2 fast |0 (OCoLC)fst00827694 | |
| 650 | 7 | |a Dynamic meteorology |x Mathematical models. |2 fast |0 (OCoLC)fst00900287 | |
| 700 | 1 | |a Stashchuk, Nataliya. | |
| 700 | 1 | |a Hutter, Kolumban. | |
| 776 | 0 | 8 | |i Print version: |a Vlasenko, Vasiliy. |t Baroclinic tides. |d New York : Cambridge University Press, 2005 |z 0521843952 |w (DLC) 2005053166 |w (OCoLC)61278693 |
| 856 | 4 | 0 | |u https://ebsco.uam.elogim.com/login.aspx?direct=true&scope=site&db=nlebk&AN=138978 |z Texto completo |
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| 938 | |a ProQuest MyiLibrary Digital eBook Collection |b IDEB |n 41598 | ||
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| 938 | |a YBP Library Services |b YANK |n 3275612 | ||
| 994 | |a 92 |b IZTAP | ||