1. Strong bottom currents in large, deep Lake Geneva generated by higher vertical-mode Poincaré waves.
- Author
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Reiss RS, Lemmin U, Monin C, and Barry DA
- Abstract
Although internal seiches are ubiquitous in large, deep lakes, little is known about the effect of higher vertical-mode seiches on deepwater dynamics. Here, by combining entire summer season current and temperature observations and 3D numerical modeling, we demonstrate that previously undetected vertical mode-two and mode-three Poincaré waves in 309-meter deep Lake Geneva (Switzerland/France) generate bottom-boundary layer currents up to 4 cm s
-1 . Poincaré wave amphidromic patterns revealed three strong cells excited simultaneously. Weak hypolimnetic stratification ( N2 ≈ 10-6 s-2 ), typical of deep lakes, significantly modified the wave structure by shifting the lower vertical node in the lake's center from ~75-meter depth (without stratification) to ~150-meter depth (with stratification). This shift induces shear in the middle of the hypolimnion and strengthens bottom currents, with important implications for hypolimnetic mixing and sediment-water exchange. Our findings demonstrate that classical concepts based on constant temperature layers cannot correctly characterize higher vertical-mode Poincaré seiches in deep lakes., Competing Interests: Competing interestsThe authors declare no competing interests., (© The Author(s) 2024.)- Published
- 2024
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