be to determine the percent removed based on the direction of longshore
transport when a rip current is present.
References
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sediment transport in a rip channel," Marine Geology 140, 25-45.
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zone: Response to incident wave and longshore current interaction," Marine
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Brander, R. W. (1999a). "Field observations on morphodynamic evolution of a
low-energy rip current system," Marine Geology 157, 199-217.
Brander, R. W. (1999b). "Sediment transport in low-energy rip current systems,"
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Brander, R. W., and Short, A. D. (2000). "Morphodynamics of a large-scale rip
current system at Muriwai Beach, New Zealand," Marine Geology 165, 27-
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Bowen, A. J., and Inman, D. L. (1969). "Rip currents II," Journal of Geophysical
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Cook, D. O. (1970). "The occurrence and geologic work of rip currents off
Southern California," Marine Geology 9, 173-186.
Dalrymple, R. A. (1975). "A mechanism for rip current generation on an open
coast," Journal of Geophysical Research 80, 3,485-3,487.
Dalrymple, R. A. (1978). "Rip currents and their causes," Proceedings 16th
Coastal Engineering Conference, American Society of Civil Engineers
(ASCE), 1,414-1,427.
Dalrymple, R. A., and Lozano, C. J. (1978). "Wave-current interaction models
for rip currents," Journal of Geophysical Research 83, 6,063-6,071.
Dolan, T. J., Castens, P. G., Sonu, C. J., and Egense, A. K. (1987). "Review of
sediment budget methodology: Oceanside littoral cell, California,"
Proceedings Coastal Sediments '87, ASCE, 1,289-1,304.
Fowler, R. E., and Dalrymple, R. A. (1990). "Wave group forced nearshore
circulation," Proceedings 22nd Coastal Engineering Conference, ASCE, 729-
742.
C12
Appendix C
Literature Review of Cross-Shore Transport by Rip Currents