1 edition of **Dynamics of Internal Gravity Waves in the Ocean** found in the catalog.

- 90 Want to read
- 31 Currently reading

Published
**2001**
by Springer Netherlands in Dordrecht
.

Written in English

- Global analysis (Mathematics),
- Oceanography,
- Geography

This monograph creates a systematic interpretation of the theoretical and the most actual experimental aspects of the internal wave dynamics in the ocean. Firstly, it draws attention to the important physical effects from an oceanographical point of view which are presented in mathematical descriptions. Secondly, the book serves as an introduction to the range of modern ideas and the methods in the study of wave processes in dispersive media. The book is meant for specialists in physics of the ocean, oceanography, geophysics, hydroacoustics.

**Edition Notes**

Statement | by Yu. Z. Miropol"sky ; edited by O. D. Shishkina |

Series | Atmospheric and Oceanographic Sciences Library -- 24, Atmospheric and Oceanographic Sciences Library -- 24 |

Contributions | Shishkina, O. D. |

Classifications | |
---|---|

LC Classifications | GC1-1581 |

The Physical Object | |

Format | [electronic resource] / |

Pagination | 1 online resource (xvii, 406 p.) |

Number of Pages | 406 |

ID Numbers | |

Open Library | OL27033528M |

ISBN 10 | 9048156920, 9401713251 |

ISBN 10 | 9789048156924, 9789401713252 |

OCLC/WorldCa | 851370249 |

If generated in the ocean by tidal flow over submarine ridges or the continental shelf, they are called internal tides. If they evolve slowly compared to the Earth's rotational frequency so that their dynamics are influenced by the Coriolis effect, they are called inertia gravity waves or, simply, inertial waves. In fluid dynamics, gravity waves are waves generated in a fluid medium or at the interface between two media when the force of gravity or buoyancy tries to restore equilibrium. An example of such an interface is that between the atmosphere and the ocean, which gives rise to wind waves.

Scripps Institution of Oceanography University of California, San Diego. Preface Wind waves, with periods of a few seconds, and the tides, with periods of You can nd lots of books about ocean waves. Nearly all of them fall g= m sec 2 is the gravity constant, and tanh(s) = e s e e s+ e (). INTERNAL GRAVITY WAVES The study of internal gravity waves provides many challenges: they move along interfaces as well as in fully three-dimensional space, and they do so at relatively.

Atmosphere-Ocean Dynamics Dynamic Meteorology ESS Prof. Jin-Yi Yu Waves in the Atmosphere and Oceans •External gravity wave (Shallow-water gravity wave) •Internal gravity (buoyancy) wave •Inertial-gravity wave: Gravity waves that have a large enough wavelength to . Internal gravity waves Internal waves are waves which, as the name suggests, occur in the interior of a fluid. You may be asking what sort of restoring force makes waves in the interior of a fluid possible, or you may question how important waves which do not occur on the surface of a fluid are.

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Journal of Geophysical, Astrophysical and Fluid Dynamics, () 'It is probable that here we may have a new classic in the field Dynamics of Internal gravity Waves in the Ocean should be in the library of every fluid dynamicist and dynamical oceanographer or meteorologist.'.Cited by: ' It is probable that here we may have a new classic in the field Dynamics of Internal gravity Waves in the Ocean should be in the library of every fluid dynamicist and dynamical oceanographer or.

This monograph creates a systematic interpretation of the theoretical and the most actual experimental aspects of the internal wave dynamics in the ocean. Firstly, it draws attention to the important physical effects from an oceanographical point of view which are presented in mathematical descriptions.

The book "Dynamics of the Internal Gravity Waves in the Ocean" considers modern theoretical methods of investigating wave motions, results of their application to internal waves problems.

describe the internal gravity wave dynamics in the ocean. Our numerical and analytical results show that the internal gravity waves have a significant impact on underwater objects in the ocean. Key words: Stratified ocean, internal gravity waves, asymptotic methods. Abstract: In this paper we consider fundamental processes of the disturbance and propagation of internal gravity waves in the ocean modeled as a vertically stratified, horizontally non-uniform, and non-stationary medium.

We develop asymptotic methods for describing the wave dynamics by generalizing the spatiotemporal ray-tracing method (a geometrical optics method).Cited by: 1. Jul 30, · Internal gravity waves occur in the atmosphere and oceans as a result of their internal density stratification.

In the atmosphere, the flow is sometimes visualized naturally by rows of cloud bands, condensation regions near the wave crests.

In the oceans, they have excited intense interest because of their strong effects on acoustic locopfl.com by: We demonstrate that our mathematical models can realistically describe the internal gravity wave dynamics in the ocean. Our numerical and analytical results show that the internal gravity waves.

Fundamental Problems of Internal Gravity Waves Dynamics in Ocean – Pages Vitaly V. Bulatov and Yury V. Vladimirov. Institute for Problems in Mechanics RAS, Pr. Near-Inertial Internal Gravity Waves in the Ocean Matthew H.

Alford, 1Jennifer A. MacKinnon, Harper L. Simmons,2 and Jonathan D. Nash3 1Scripps Institution of Oceanography, University of California, San Diego, La Jolla, California ; email: [email protected] 2School of Fisheries and Ocean Sciences, University of Alaska at Fairbanks, Fairbanks.

"Pedlosky has spent his time well in writing Waves in the Ocean and Atmosphere. The writing is informal and engaging. the clarity of the figures and text is uniformly high.

my message to students and researchers working in the fields of atmospheric and oceanic dynamics is ‘buy this book’.Cited by: pt. Principles of thermohydrodynamic description of internal gravity waves in the ocean.

Brief Information About Oceanic Thermohydrodynamic. Equations of the Theory of Internal Waves --pt. Linear theory of internal waves.

Linear Theory of Propagation of Internal Waves in the Undisturbed Horizontally Homogeneous Ocean. Mar 09, · This monograph creates a systematic interpretation of the theoretical and the most actual experimental aspects of the internal wave dynamics in the ocean.

Firstly, it draws attention to the important physical effects from an oceanographical point of Brand: Springer Netherlands. Dynamics of Internal Gravity Waves in the Ocean. [Yu Z Miropol'sky; O D Shishkina] -- This monograph creates a systematic interpretation of the theoretical and the most actual experimental aspects of the internal wave dynamics in the ocean.

Nov 01, · This video is unavailable. Watch Queue Queue. Watch Queue Queue. This book contains a comprehensive study of the internal ocean waves, which play a very important role in ocean physics providing mechanisms for ocean water mixing and circulation, as well as the transportation of gases, nutrients, and a very large number of marine organisms in the ocean body.

Jun 03, · Atmosphere-Ocean Dynamics deals with a systematic and unified approach to the dynamics of the ocean and atmosphere. The book reviews the relationship of the ocean-atmosphere and how this system functions.

The text explains this system through radiative equilibrium models; the book also considers the greenhouse effect, Book Edition: 1. The study of internal gravity waves provides many challenges: they move along interfaces as well as in fully three-dimensional space, at relatively fast temporal and small spatial scales, making them difficult to observe and resolve in weather and climate models.5/5(1).

Nonlinear interactions among internal gravity waves. Abstract. This paper reviews the nonlinear interaction calculations for the internal gravity wave field in the deep ocean.

The nonlinear interactions are a principal part of the dynamics of internal waves and are an important link in the overall energy cascade from large to small locopfl.com by: We present analytical and numerical algorithms for calculating the internal gravity wave fields using actual ocean parameters such as physical characteristics of the sea water, topography of its floor, etc.

We demonstrate that our mathematical models can realistically describe the internal gravity wave dynamics in the locopfl.com: Vitaly V. Bulatov and Yuriy V. Vladimirov. The former leads to internal gravity waves (and surface gravity waves as well).

Internal gravity waves are simpler to un derstand and clearly manifest the various ways in which waves interact with the mean state.

For reasons which will soon become clear, internal gravity waves are not a dominant part of the midlatitude tropospheric circulation.There will be two projects on surface gravity and internal waves with a goal to either confirm or reject the theoretical constructs you're learning.

The final grade will be based 1/2 on problem sets (HW + quizes), 1/4 on projects and 1/4 on final exam.The uniform asymptotic form of the internal gravity waves field generated by a source moving above the smoothly varying bottom is constructed.

The problem of reconstructing non-harmonic internal gravity wave packets generated by a source moving in a stratified ocean is considered.

The solution is proposed in terms of wave modes, propagating independently at the adiabatic approximation, and.