Coastal Restoration Trust of New Zealand

Coastal Dune Ecosystem Reference Database

Factor controlling the entrance cross-sectional area off four inlets (Note) Journal Paper

Author
Heath, R.A.
Year
1976
Journal / Source
New Zealand Journal of Marine and Freshwater Research
Volume
10
Pages
725-735
Keywords
tidal asymmetry, sediment movement, North Cape, Foveaux Strait, Cook Strait, Marlborough Sounds
Summary
Available tidal observations indicate a significant asymmetry in the tide around northernmost New Zealand and in Cook and Foveaux Straits. However only around northernmost New Zealand does the tidal asymmetry dominate the time-averaged mean flow and determine the direction of peak flow; there the tidal asymmetry may have a strong influence on the present development of Pandora Bank. The relatively large MiM2 tidal elevations in Cook Strait lead to significant tidal asymmetry in the Marlborough Sounds, with the ebb speeds exceeding the flood, and they play an important role in determining the direction of net bedload sediment transport