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- W4381415392 abstract "A near-equatorial solution forced by periodic winds is obtained to the complete LCS equations. It is found assuming that the Coriolis parameter is $$f=beta y$$ , allowing it to be represented as an expansion in Hermite functions. The same processes identified in the previous chapter for switched-on winds occur in the periodic one, except that they happen continuously rather then sequentially. When there is an eastern boundary, the wind-forced equatorial Kelvin wave reflects as a packet of Rossby and evanescent waves, with Rossby waves existing only equatorward of the critical latitude $$theta _{cr}$$ , and evanescent ones superposing to form a $$beta $$ -plane Kelvin wave north of $$theta _{cr}$$ . With both boundaries, two types of resonant responses are possible: “equatorial basin resonance,” which is linked to the natural ringing time of the basin; and “zero-group-velocity” resonance that occurs when the ocean is forced at the critical frequency of an Rossby or gravity wave." @default.
- W4381415392 created "2023-06-21" @default.
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- W4381415392 date "2023-01-01" @default.
- W4381415392 modified "2023-09-23" @default.
- W4381415392 title "Equatorial Ocean: Periodic Forcing" @default.
- W4381415392 doi "https://doi.org/10.1007/978-981-19-5864-9_15" @default.
- W4381415392 hasPublicationYear "2023" @default.
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