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Fig. 11-CO, p. 297

Fig. 11-CO, p. 297. Fig. 11-1a, p. 299. Fig. 11-1b, p. 299. Fig. 11-2a, p. 300. Fig. 11-2b, p. 300. Fig. 11-2c, p. 300. Motion due to inertia. Combined effect. Motion due to gravity. c. Fig. 11-2c, p. 300. Fig. 11-3, p. 300. 1,650 km (1,023 mi).

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Physical Oceanography

Physical Oceanography. Tides. Tides. Tides are caused by the gravitational force of the moon and sun and the motion of earth. The wavelength of tides can be half the circumference of earth. Tides are forced waves because they are never free of the forces that cause them.

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Higher low tide - PowerPoint PPT Presentation

Fig. 11-CO, p. 297

Physical Oceanography