By M. Schwartz
ISBN-10: 1402019033
ISBN-13: 9781402019036
Maurice Schwartz, Editor of the a lot acclaimed Encyclopedia of shores and Coastal Environments (Hutchinson Ross, 1982) has now introduced forth a brand new quantity with a clean interdisciplinary method that comes with geomorphology, ecology, engineering, know-how, oceanography, and human actions as they relate to coasts. inside its covers the Encyclopedia of Coastal technology contains many facets of the coastal sciences which are merely to be chanced on scattered between medical literature.
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Extra info for Encyclopedia of Coastal Science (Encyclopedia of Earth Sciences Series)
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Lowest salinity in coastal waters is therefore in the Gulf of Guinea and highest values are in the Red Sea. The coasts of Africa experience semi-diurnal tides, with the exception of the east coast of Madagascar, the horn and the Mediterranean coast of Egypt, where tides are mixed. Spring tide range mostly approximates 2 m, except in the Mozambique Channel where it is larger and can exceed 4 m, and along the Red Sea and Mediterranean coasts where tides are small (Davies, 1972). The entire east coast experiences temperatures permanently above 20ЊC, as does the central west coast.
Spring tide range mostly approximates 2 m, except in the Mozambique Channel where it is larger and can exceed 4 m, and along the Red Sea and Mediterranean coasts where tides are small (Davies, 1972). The entire east coast experiences temperatures permanently above 20ЊC, as does the central west coast. Upwelling in the southwest and northwest lowers temperatures regionally. Major currents are the Somali and Mozambique/Agulhas in the east and the Benguella, Guinea, and Canary currents in the west.
5 km/yr during the first year (Hicks and Inman, 1987). 8 km/yr (Table A1). It has been observed that any structure that interrupts the littoral drift of sand along a beach results in an erosional chain reaction traveling downdrift from the structure (Inman and Brush, 1973). The propagation rates of the downdrift erosion wave was evaluated from beach Background The concept of an accretion/erosion wave was developed to account for the downdrift movement of a sand delta deposited across the beach by an ephemeral stream (Inman and Bagnold, 1963).
Encyclopedia of Coastal Science (Encyclopedia of Earth Sciences Series) by M. Schwartz
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