DSTL (PDF) - Cham

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Figure 6. (Top left) PHOENICS wave profile predictions for the 100m initial wave att=21250s compared with observations (top right, Orr and Mignerey, 2003) from ADCPbackscatter intensity. Waves are travelling from left to right. (Bottom left) PHOENICS rangevelocity comparison for the 100m initial wave at t=21250s with ADCP (bottom right, Orr andMignerey private communication) range velocity measurements.12
Figure 7. (Top) PHOENICS predictions of log10 of the rate of dissipation of turbulent kineticenergy per unit mass at t=21250s (scale range is –9.05 to –3.84). Density contours relative to1000 kg/m 3 are superimposed to illustrate the wave shape in relation to the dissipationpredictions. (Bottom) Gradient Richardson number plot.13
Page 1 and 2: Title: Some applications of PHOENIC
Page 3 and 4: profiles taken during the experimen
Page 5 and 6: athymetry (first case study) is not
Page 7 and 8: Figure 1. (Top) Bathymetry of South
Page 9 and 10: Figure 3. 100m amplitude wave case.
Page 11: Figure 5. (Top)Variation of wave ph
Page 15 and 16: Figure 9. Turbulent dissipation rat
Page 17 and 18: Figure 11. (Top) Predicted concentr
Page 19 and 20: Figure 13. Malin shelf internal wav

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