Spectral evolution of wind-generated surface gravity waves in a dispersed ice field

[1]  B. Golding,et al.  A wave prediction system for real-time sea state forecasting , 1983 .

[2]  V. Squire Numerical Modelling of Realistic Ice Floes in Ocean Waves , 1983, Annals of Glaciology.

[3]  T. Barnett,et al.  Measurements of wind-wave growth and swell decay during the Joint North Sea Wave Project (JONSWAP) , 1973 .

[4]  Peter Wadhams,et al.  A mechanism for the formation of ice edge bands , 1983 .

[5]  S. Hasselmann,et al.  Computations and Parameterizations of the Nonlinear Energy Transfer in a Gravity-Wave Spectrum. Part I: A New Method for Efficient Computations of the Exact Nonlinear Transfer Integral , 1985 .

[6]  P. Wadhams Airborne laser profiling of swell in an open ice field , 1975 .

[7]  D. Webb,et al.  Non-linear transfers between sea waves , 1978 .

[8]  Klaus Hasselmann,et al.  A parametric wave prediction model , 1976 .

[9]  K. Hasselmann On the non-linear energy transfer in a gravity-wave spectrum Part 1. General theory , 1962, Journal of Fluid Mechanics.

[10]  O. Phillips Spectral and statistical properties of the equilibrium range in wind-generated gravity waves , 1985, Journal of Fluid Mechanics.

[11]  K. Hasselmann,et al.  On the Existence of a Fully Developed Wind-Sea Spectrum , 1984 .

[12]  M. Fox On the nonlinear transfer of energy in the peak of a gravity-wave spectrum. II , 1976, Proceedings of the Royal Society of London. A. Mathematical and Physical Sciences.

[13]  D.J.T. Carter,et al.  Prediction of wave height and period for a constant wind velocity using the JONSWAP results , 1982 .

[14]  J V Wehausen,et al.  THE MOTION OF FLOATING BODIES , 1971 .

[15]  P. Wadhams Attenuation of swell by sea ice , 1973 .

[16]  Michael Selwyn Longuet-Higgins,et al.  On the nonlinear transfer of energy in the peak of a gravity-wave spectrum: a simplified model , 1976, Proceedings of the Royal Society of London. A. Mathematical and Physical Sciences.

[17]  K. Hasselmann On the non-linear energy transfer in a gravity-wave spectrum. Part 3. Evaluation of the energy flux and swell-sea interaction for a Neumann spectrum , 1963, Journal of Fluid Mechanics.

[18]  An operational coupled hybrid wave prediction model , 1984 .

[19]  John D. Fenton,et al.  Wave forces on vertical bodies of revolution , 1978, Journal of Fluid Mechanics.

[20]  M. Isaacson Fixed and Floating Axisymmetric Structures in Waves , 1982 .

[21]  G. Robin Wave propagation through fields of pack ice , 1963, Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences.

[22]  R. Long,et al.  Array measurements of atmospheric pressure fluctuations above surface gravity waves , 1981, Journal of Fluid Mechanics.

[23]  Klaus Hasselmann,et al.  On the spectral dissipation of ocean waves due to white capping , 1974 .

[24]  O. Phillips On the dynamics of unsteady gravity waves of finite amplitude Part 1. The elementary interactions , 1960, Journal of Fluid Mechanics.

[25]  M. Donelan,et al.  Directional spectra of wind-generated ocean waves , 1985, Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences.

[26]  V. Squire A theoretical, laboratory, and field study of ice‐coupled waves , 1984 .

[27]  P. Wadhams,et al.  The Effect of the Marginal Ice Zone on the Directional Wave Spectrum of the Ocean , 1986 .

[28]  J. Miles A note on variational principles for surface-wave scattering , 1971, Journal of Fluid Mechanics.

[29]  Fritz John,et al.  On the motion of floating bodies II. Simple harmonic motions , 1950 .

[30]  K. Hasselmann,et al.  Computations and Parameterizations of the Nonlinear Energy Transfer in a Gravity-Wave Specturm. Part II: Parameterizations of the Nonlinear Energy Transfer for Application in Wave Models , 1985 .

[31]  Walter B. Tucker,et al.  Physical properties of summer sea ice in the Fram Strait, June-July, 1984 , 1987 .

[32]  Seelye Martin,et al.  Field Observations of the Bering Sea Ice Edge Properties during March 1979 , 1980 .