Practical Methods for Observing and Forecasting Ocean Waves by Means of Wave Spectra and Statistics

Practical Methods for Observing and Forecasting Ocean Waves by Means of Wave Spectra and Statistics
Author: Willard J Pierson (Jr)
Publisher:
Total Pages: 299
Release: 1971
Genre:
ISBN:

;Contents: The properties of ocean waves; The generation and forecasting of sea waves; Wave propagation and forecasting swell waves--simple models; Wave observation techniques; Synoptic forecasting methods and weather map analysis; Wave refraction; Operational applications of forecasting methods; Verification by forecasts and observations.

Maritime Engineering and Technology

Maritime Engineering and Technology
Author: Carlos Guedes Soares
Publisher: CRC Press
Total Pages: 698
Release: 2012-11-26
Genre: Technology & Engineering
ISBN: 0203105184

Maritime Engineering and Technology includes the papers from the 1st International Conference on Maritime Technology and Engineering (MARTECH 2011, Lisbon, Portugal, 10-12 May 2011). MARTECH 2011 was held to commemorate 100 years of the Instituto Superior Tico (IST) in Lisbon, and the contributions in the present volume reflect the

Coastal Engineering - Waves, Beaches, Wave-Structure Interactions

Coastal Engineering - Waves, Beaches, Wave-Structure Interactions
Author: T. Sawaragi
Publisher: Elsevier
Total Pages: 497
Release: 1995-04-11
Genre: Technology & Engineering
ISBN: 0080544843

The science and technology of coastal and ocean engineering are closely related to harbour and fishery engineering, because they share a common basic knowledge. However, whereas various publications of coastal engineering, harbour engineering, and ocean engineering have described just the knowledge in their own respective fields, an interrelated and systematic presentation linking them together has yet to be attempted. This book is the first attempt to systematically combine the fields of coastal, ocean, harbour, and fishery engineering from an engineering viewpoint backed by hydrodynamics. Understanding the interaction of waves with structures and sediment, and predicting the associated responses of interest, underlie nearly every problem in coastal and ocean engineering. This is precisely the goal of this book. Although primarily intended for use as a special textbook for graduate students and senior practising engineers, it is hoped that this book will also serve as a useful reference and assist in the further development of this field. With these objectives in mind, each chapter deals with important problems to be solved in the near future. The references included in each chapter should aid students and practising engineers in further broadening their knowledge.This book is the English translation of the original Japanese version published in May, 1991, commemorating the author's retirement from Osaka University. ``Elsevier will be named copyright holder of the English translated publication of the Work. This grant by Gihodo Publishers Ltd. (GP) only pertains to the English language version of the Work and no other rights, except to publish the Work in the English language, are granted to Elsevier Science (ES) by GP, which is acknowledged by ES to be the original copyright holder in the Work.''

Geophysik II / Geophysics II

Geophysik II / Geophysics II
Author:
Publisher: Springer Science & Business Media
Total Pages: 1054
Release: 2012-12-06
Genre: Science
ISBN: 3642458815

45 downwards because (j on the average increases with height; but this conclusion does not follow from (18.3) when the dependency of Kc upon ~o is taken into consideration. s 2 ERTELl and PRIESTLEY and SWINBANK have shown that the upward eddy flux of sensible heat must be larger than indicated by (18.3), because this formula does not account for the fact that rising eddies are systematically warmer than sinking eddies because of the effect of buoyancy. The reader is referred to the reviews by SUTTON [22], [23] and PRIESTLEY and SHEP PARD [15) for further details concerning eddy-flux of heat and turbulent diffusion. 19. RICHARDSON'S criterion. The right-hand side of (15.10) represents the rate of production of eddy energy. The last term represents energy loss by dissipation; in order that the eddy energy shall be maintained, it is therefore necessary that P div V" - (! V" v" . grad. v > O.