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- W2008397044 abstract "Current meters moored for 19.5 months at Lat. 20°S in the deep water of the western Mascarene Basin recorded a distinct, large-amplitude [O(10cms−1)] undulation of bimonthly period, propagating westward at 7cms−1. Its characteristics demonstrate that it was a barotropic Rossby wave of relatively large meridional scale. Simple theory accounts for it as having been forced by local wind-stress curl at one of the resonant frequencies of the Mascarene Basin. A sharp bimonthly peak is also prominent in spectra of TOPEX/POSEIDON sea-surface height in the Mascarene Basin, but is not seen to the eastward, as is consistent with the local generation. Fluctuations of 45-day period reported earlier in the upper ocean just northeast of Madagascar might have been generated through a similar process, but with frequency shifted by the South Equatorial Current." @default.
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- W2008397044 date "2002-01-01" @default.
- W2008397044 modified "2023-10-16" @default.
- W2008397044 title "Forced resonant undulation in the deep Mascarene Basin" @default.
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- W2008397044 doi "https://doi.org/10.1016/s0967-0645(01)00151-5" @default.
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