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- W2067709636 abstract "A sharp decrease in the semi-diurnal tidal admittances around New Zealand occurs for constituents with periods less than 12.19 h. The situation is epitomized here by analysis of the principal lunar (M2) and solar (S2) constituents, the admittance of S2 being significantly smaller than that of M2. Incident tidal energy from the northeast of New Zealand gives rise to trapped progressive wave components moving anti-clockwise around the coast, whereas incident tidal energy from the northwest gives rise to standing wave components on the west coast. Differences in the relative strength of the tidal energy incident on New Zealand from different directions result initially from spatial differences in the tidal distribution of the semi-diurnal constituents in the Pacific Ocean further north. The M2 tide has a dominant trapped progressive wave component around New Zealand whereas on the west coast the S2 standing wave component is slightly larger than the small progressive wave component. Little of the standing wave component energy on the west coast is transmitted around southern New Zealand to the east coast, and this leads to the observed decrease in the S2 tidal admittance from the west to the east coast." @default.
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- W2067709636 date "1981-08-01" @default.
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- W2067709636 title "Variations of the semi-diurnal tidal admittance near New Zealand" @default.
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- W2067709636 doi "https://doi.org/10.1016/s0198-0149(81)80004-0" @default.
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