A numerical model for shore‐normal sediment size variation on a macrotidal beach
- 1 December 1992
- journal article
- research article
- Published by Wiley in Earth Surface Processes and Landforms
- Vol. 17 (8) , 755-773
- https://doi.org/10.1002/esp.3290170804
Abstract
No abstract availableKeywords
This publication has 43 references indexed in Scilit:
- Supplement to a paper on the Theory of Oscillatory WavesPublished by Cambridge University Press (CUP) ,2010
- A note on suspension transport in the beach gradient modelEarth Surface Processes and Landforms, 1990
- Textural Variation in Sub-Environments of the Shallow-Water Wave Zone, Kouchibouguac Bay, New BrunswickCanadian Journal of Earth Sciences, 1972
- TEXTURAL DIFFERENTIATION ON THE SHORE FACE DURING EROSIONAL RETREAT OF AN UNCONSOLIDATED COAST, CAPE HENRY TO CAPE HATTERAS, WESTERN NORTH ATLANTIC SHELFSedimentology, 1971
- Tidal Cycle of Changes in an Equilibrium Beach, Sandy Hook, New JerseyThe Journal of Geology, 1966
- ENERGY MEASUREMENTS IN THE SWASH—SURF ZONE1Limnology and Oceanography, 1965
- The long-wave paradox in the theory of gravity wavesMathematical Proceedings of the Cambridge Philosophical Society, 1953
- Sorting and Transportation of Material in the Swash and BackwashJournal of Sedimentary Research, 1939
- On Sea-Beaches and Sandbanks (Continued)The Geographical Journal, 1898
- On Sea-Beaches and SandbanksThe Geographical Journal, 1898