Abstract

Abstract A series of laboratory experiments was performed in a thermally-driven rotating annulus of fluid with and without two-wave bottom topography. Velocity measurements were made by illuminating a thin layer of fluid at mid-depth and photographing successive positions of tracer particles suspended in the fluid. Streamfunctions were determined from the calculated vorticity. Comparison of the rotational velocity field with the measured velocity field revealed negligible differences, indicating that the flow was horizontally quasi-nondivergent. A detailed analysis was made of one experiment with and one without topography at the same point in dimensionless parameter space. The results indicate that the effect of topography is 1) to modulate the synoptic-scale waves in both space and time, 2) to suppress the odd modes and 3) to force a “planetary” scale mode which oscillates about a climatological mean position (with high pressure centers located in this experiment approximately 22° upstream of the mounta...

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