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- W1983196105 abstract "[1] Shipboard observations are presented that suggest the occurrence of parametric subharmonic instability (PSI) of diurnal K1 and O1 internal tides at “critical” latitudes of 14.52°N and 13.44°N, respectively. In a transect spanning 12.5–18°N, depth-mean shear squared shows sharp peaks at 14.52°N (elevated relative to that at 15°N by a factor of ten) and at 13.44°N (by a factor of 7). Wind speed measured from the ship and Quikscat scatterometer during and before the transect was <10 m s−1 at these latitudes. Eight-hour time series (about 1/6 of an inertial period) of shear and isopycnal depth at 14.52°N are sufficient to associate the elevated shear with alternating, clockwise-rotating layers analogous to those observed at the M2 critical latitude of 28.8°N." @default.
- W1983196105 created "2016-06-24" @default.
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- W1983196105 date "2008-08-05" @default.
- W1983196105 modified "2023-10-18" @default.
- W1983196105 title "Observations of parametric subharmonic instability of the diurnal internal tide in the South China Sea" @default.
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- W1983196105 doi "https://doi.org/10.1029/2008gl034720" @default.
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