Extreme Ocean Waves

Extreme, freak or rogue waves are produced by a number of physical mechanisms that focus the water-wave energy into a small area, due to wave instability, chaotic behaviour, dispersion (frequency modulation), refraction (presence of variable currents or b

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Efim Pelinovsky • Christian Kharif Editors

Extreme Ocean Waves

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Editors Efim Pelinovsky Russian Academy of Sciences Inst. Appl. Physics Ul’yanov str. 46 Nizhny Novgorod Russia 603950 [email protected]

Christian Kharif IRPHE Technopole de Chateau-Gombert 49 rue F. Joliot Curie 13384 Marseille BP 146 France [email protected]

c 2008 JupiterImages Corporation Cover images  ISBN 978-1-4020-8313-6

e-ISBN 978-1-4020-8314-3

Library of Congress Control Number: 2008928129 c 2008 Springer Science+Business Media B.V.  No part of this work may be reproduced, stored in a retrieval system, or transmitted in any form or by any means, electronic, mechanical, photocopying, microfilming, recording or otherwise, without written permission from the Publisher, with the exception of any material supplied specifically for the purpose of being entered and executed on a computer system, for exclusive use by the purchaser of the work. Printed on acid-free paper 9 8 7 6 5 4 3 2 1 springer.com

Preface

Extreme wave events occurring in seas and oceans almost every week are reported. There are a number of physical mechanisms that focus the water wave energy into a small area and produce the occurrence of extreme waves called freak or rogue waves. These events may be due to wave instability (modulation or Benjamin-Feir instability), chaotic behavior, dispersion (frequency modulation), refraction (presence of variable currents or bottom topography), soliton interactions, etc. These giant waves are a real danger to ships and platforms, causing accidents resulting in human loss. There are several examples of such events which occurred in 2007. The freak surge striking East Anglia and Kent (UK) on November 12 missed the high tide by minutes and forced the emergency services to evacuate more than 1,000 people from their homes. Strong waves struck a group of 15 picnickers who had waded far into the sea on October 15 at the Gadani beach about 40 km southwest of Karachi (Pakistan). On October 1, nine houses were destroyed and 77 families displaced when strong waves hit the coastal Davao City (Phillipine). The heavy rain and freak tides on August 31 damaged and in some cases destroyed banks and walls along the Saigon River (Vietnam). A 7–10-m wave hit many people in Mostaganem (Algeria) killing 12 on August 3. One man was killed by a freak wave while fishing on the rocks off the coast of Scotland (UK) on August 2. He was swept out to sea. A tourist was killed by a giant wave as freak weather hit the French Mediterranean island of Corsica on May 30. Great damage was caused to a large passenger ferry “L’Enez Sun III” in the English Channel near Island Sein on May 19. Such events occur in the English Channel each year. The ferry “La D´eesse des Flots” was hit by a freak wave of 10 m on August 3, 2006 near the French coast (Barfleur). The wave, estimated as 12 m high crashed into the “Pont-Aven”, the flagship of the British Ferries fleet on May 22, 2006, near the French port of Roscoff. The wave was of 12 m and five passengers we