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• W1485823458 abstract "Measurements are made in Lake Geneva to examine internal waves and flow characteristics in the stratified water overlying a 17° sloping bed in a water depth of about 30m. Even after a period of calm weather lasting three weeks, the water column is observed to be active, with internal oscillations of amplitude as great as 3 m. Internal waves are known to generate sheets and layers in the thermal structure of the water column, as described by Lazier (1973) those observed here have a predominantly downward phase propagation, indicating upward energy propagation. Such effects caused by enhanced internal wave activity through reflection near sloping boundaries may account for the increase in layering reported by Caldwell et al. (1978) as the side of a lake is approached, rather than the presence of intrusions. Internal waves with up-and down-slope currents reaching 10 cm s−1 and frequencies at, or close to, the ‘critical' frequency on the slope, are observed in the bottom two metres of the water column; fluctuations with frequencies near critical are important in determining the nature of the slope boundary layer in lakes as well as in the ocean, where internal wave amplification has been observed by Eriksen (1982). Measurements of vertical velocity using an acoustic Doppler velocity profiler in this benthic layer, and ancillary observations, reveal a density current carrying sediment-laden warm water down the slope. The current is finely layered in its velocity structure, changes occurring over vertical scales of about 10 cm." @default.
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• W1485823458 date "2013-03-19" @default.
• W1485823458 modified "2023-10-16" @default.
• W1485823458 title "Finescale Dynamics of Stratified Waters Near a Sloping Boundary of a Lake" @default.
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• W1485823458 doi "https://doi.org/10.1029/ce054p0461" @default.
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