Abstract
Flow splitting in the Rhine valley has been observed with a transportable wind lidar (TWL) during a shallow-foehn event in the framework of the Mesoscale Alpine Programme (MAP). The Doppler lidar recorded in detail flow splitting, foehn wind gusts, and flow reversal. Such structures have not previously been observed with comparable detail by conventional in-situinstruments. In addition to the TWL, boundary-layer processes have been documented by means of rawinsondes and surface stations. This paper presents an analysis of the processes giving birth to flow splitting between the Seez and Rhine valleys during Intensive Observation Period (IOP) 5 (1–3 October 1999) by combining the collected data with hydraulic theory. The study shows thatthe splitting of the channelled flow is associated with (1) the existence of a stagnation point at the intersection of the Seez and Rhine valleys, and (2) the deflection of the flow by the lateral sidewalls of the valleys.
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Drobinski, P., Dabas, A.M., Haeberli, C. et al. On The Small-Scale Dynamics Of Flow Splitting In The Rhine Valley During A Shallow Foehn Event. Boundary-Layer Meteorology 99, 277–296 (2001). https://doi.org/10.1023/A:1018925930339
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DOI: https://doi.org/10.1023/A:1018925930339