Internal wave weather heterogeneity in a deep multi-basin subalpine lake resulting from wavelet transform and numerical analysis

The internal wave-field of a Y-shaped lake (Lake Como, North Italy) was investigated over a 3-year long
period applying wavelet time–frequency analysis to temperature and wind data time series, recorded at
the edge of each of the three arms. The comparison with the results from a modal model allowed to iden-
tify the presence of both first and second vertical modes of oscillations. The field data analysis underlined
a heterogeneous baroclinic response with the eastern arm decoupled from the remaining part of the lake
constituted by the northern and western arms (north–south west transect). This disjoined response is
expected to enhance the water exchange between the northern and the western arm, with relevant con-
sequences on the inter-basins water exchanges and on the distribution of chemical and biological species.
In the north–south west transect the analysis of the low power signals in winter underlined a residual
internal wave activity ascribed to the first vertical free mode of oscillation (V1H1)