Finite‐floe wave reflection and transmission coefficients from a semi‐infinite model
- 15 July 1993
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research: Oceans
- Vol. 98 (C7) , 12537-12542
- https://doi.org/10.1029/93jc00940
Abstract
No abstract availableThis publication has 14 references indexed in Scilit:
- Strain in shore fast ice due to incoming ocean waves and swellJournal of Geophysical Research: Oceans, 1991
- Wave propagation in the marginal ice zone: Model predictions and comparisons with buoy and synthetic aperture radar dataJournal of Geophysical Research: Oceans, 1991
- A modal analysis of a rectangular plate floating on an incompressible liquidJournal of Sound and Vibration, 1990
- Reflection and transmission characteristics at the edge of shore fast sea iceJournal of Geophysical Research: Oceans, 1990
- The attenuation rates of ocean waves in the marginal ice zoneJournal of Geophysical Research: Oceans, 1988
- Wave Attenuation and Wave Drift in the Marginal Ice ZoneJournal of Physical Oceanography, 1987
- The Effect of the Marginal Ice Zone on the Directional Wave Spectrum of the OceanJournal of Physical Oceanography, 1986
- Direct measurement of the attenuation of ocean waves by pack iceNature, 1980
- Attenuation of swell by sea iceJournal of Geophysical Research, 1973
- Wave propagation through fields of pack icePhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1963