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and y = 2(acoshwH —wsinhwH). The equivalent expres sions for R and T for finite depth H are thus

Figure 5 and y = 2(acoshwH —wsinhwH). The equivalent expres sions for R and T for finite depth H are thus

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Copyright 1994 by the American Geophysical Union.
Copyright 1994 by the American Geophysical Union.
‘igure 1. Schematic diagram showing the geometry of the problem and the coordinate system usec
‘igure 1. Schematic diagram showing the geometry of the problem and the coordinate system usec
‘igure 1. Schematic diagram showing the geometry of the problem and the coordinate system usec
‘igure 1. Schematic diagram showing the geometry of the problem and the coordinate system usec
and y = 2(acoshwH —wsinhwH). The equivalent expres sions for R and T for finite depth H are thus
and y = 2(acoshwH —wsinhwH). The equivalent expres sions for R and T for finite depth H are thus
Figure 4. The heave response (RAO) for ice floes of different length (marked on each curve) at a constant thickness of 1m.
Figure 4. The heave response (RAO) for ice floes of different length (marked on each curve) at a constant thickness of 1m.
Figure 4. The heave response (RAO) for ice floes of different length (marked on each curve) at a constant thickness of 1m.
Figure 4. The heave response (RAO) for ice floes of different length (marked on each curve) at a constant thickness of 1m.
Figure 8. Equivalent plots to Figure 6 for a 100-mx1-m ice floe. igure 7. Equivalent plots to Figure 6 for a 50-mx1-m ice floe. Figure9. Equivalent _ e. Figure 9. Equivalent plots to Figure 6 for a 200-mx1-m ice floe
Figure 8. Equivalent plots to Figure 6 for a 100-mx1-m ice floe. igure 7. Equivalent plots to Figure 6 for a 50-mx1-m ice floe. Figure9. Equivalent _ e. Figure 9. Equivalent plots to Figure 6 for a 200-mx1-m ice floe
Figure 8. Equivalent plots to Figure 6 for a 100-mx1-m ice floe.
Figure 8. Equivalent plots to Figure 6 for a 100-mx1-m ice floe.
Figure 8. Equivalent plots to Figure 6 for a 100-mx1-m ice floe.
Figure 8. Equivalent plots to Figure 6 for a 100-mx1-m ice floe.
Figure 11. Aerial photograph of Greenland Sea MIZ sea ice, with the 50-m-long ship Polarbjgrn near the center. The photograph was taken during the 1983 Marginal Ice Zone Experiment.
Figure 11. Aerial photograph of Greenland Sea MIZ sea ice, with the 50-m-long ship Polarbjgrn near the center. The photograph was taken during the 1983 Marginal Ice Zone Experiment.
At finite depth the solution is similar, with each i cos a(€— r) term divided by a factor (tanh kH + kHsech*kH ).
At finite depth the solution is similar, with each i cos a(€— r) term divided by a factor (tanh kH + kHsech*kH ).
Figure 14. Difference between the complete two-floe theory and the noninteractive theory.
Figure 14. Difference between the complete two-floe theory and the noninteractive theory.
Figure 12. Schematic showing two adjacent floes and their respective reflection and transmission coefficients ir noninteractive solitary floe theory.
Figure 12. Schematic showing two adjacent floes and their respective reflection and transmission coefficients ir noninteractive solitary floe theory.
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