Wave Kinematics and Environmental Forces

Papers presented at a conference organized by the Society for Underwater Technology and held in London, U.K., March 24–25, 1993

  • Authors
  • Society for Underwater Technology (SUT)

Table of contents

  1. Front Matter
    Pages i-viii
  2. Wave Kinematics

    1. Front Matter
      Pages 1-1
    2. I. Cummins, C. Swan
      Pages 35-51
    3. Ove T. Gudmestad, Sverre Haver
      Pages 75-99
    4. D. J. Skyner, W. J. Easson
      Pages 101-113
    5. Hemming A. Schäffer
      Pages 115-139
  3. Fluid Loading

    1. Front Matter
      Pages 141-141
    2. J. J. Murray, R. G. Standing, L. M. Mak
      Pages 161-189
    3. M. J. Downie, B. A. Murray, P. Bettess, J. V. Haswell
      Pages 191-207
    4. M. M. Zdravkovich, J. L. Baldaro
      Pages 239-247
  4. Coastal Conditions

    1. Front Matter
      Pages 249-249
    2. H. N. Southgate
      Pages 251-273
    3. K. She, C. A. Greated, W. J. Easson
      Pages 275-287
    4. S. Lloyd, C. Greated, W. Easson
      Pages 307-316
    5. B. Li, C. A. Fleming
      Pages 317-327

About this book


In determining the response of offshore structures, it is of utmost importance to determine, in the most correct manner, all factors which contribute to the total force acting on these structures. Applying the Morison formula (Morison et. al. , 1950) to calculate forces on offshore slender structures, uncertainties related to the understanding of the wave climate, the hydrodynamic force coefficients and the kinematics of ocean waves represent the most important contributions to the uncertainties in the prediction of the total forces on these structures (Haver and Gudmestad, 1992). Traditional calculation of forces on offshore structures involves the use of regular waves with the following non-linearities inco1porated use of regular wave theories inco1porating higher order terms use of Morison equation having a nonlinear drag term inclusion of the effect of the free surface by integrating all contributions to total forces and moments from the sea floor to the free surface of the waves In order to describe the sea more realistically, the ocean surface is to be described as an irregular sea surface represented by its energy spectrum. The associated decomposition of the sea surface is given as a linear sum of linear waves. The total force is found by integrating the contribution from all components in the wave spectrum to the free surface. The kinematics of each component must therefore be determined.


Vibration kinematics model modeling wind

Bibliographic information

  • DOI
  • Copyright Information Springer Science+Business Media B.V. 1993
  • Publisher Name Springer, Dordrecht
  • eBook Packages Springer Book Archive
  • Print ISBN 978-90-481-4250-7
  • Online ISBN 978-94-017-3663-3
  • Series Print ISSN 0952-1798
  • Buy this book on publisher's site
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