H125-02
Vertically Propagating Internal Waves in a Tropical Reservoir
Abstract:
The study site is La Fe reservoir, a tropical Colombian reservoir. The main measurements were obtained from a thermistor chain located in the deepest zone of the lake. Phase analysis of the measured and simulated (AEM3D) lake temperatures revealed a gradual phase shifting along the water column for diurnal oscillations, which according to HD2012 is the signature of vertical propagation. The modeled velocities adjusted well to WKB theory of propagating internal waves.
We performed numerical experiments of periodically forced wedge-shaped basins varying the bottom slope and considering stratifications with thin and thick metalimnions, typical of summer temperate and tropical lakes, respectively. For subcritical slopes, standing seiches develop accordingly to the classical picture with phase shifts of π radians. For supercritical slopes, less energy reflects upwards to conform the standing seiche resulting in a net downward energy propagation, whose signature is the gradual upward phase shift. The signature of such effect is more evident for a wide metalimnion.
Henderson, S. M., and Deemer, B. R. (2012), Vertical propagation of lakewide internal waves, Geophys. Res. Lett., 39, L06405
Thorpe, S.A. (2013), Some Dynamical Effects of Internal Waves and the Sloping Sides of Lakes, in Physical Processes in Lakes and Oceans, Coastal Estuarine Stud., vol 54, edited by J. Imberger, pp 441-460