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Observations of a mountain-wave event over the Pyrenees
1986
Tellus: Series A, Dynamic Meteorology and Oceanography
An analysis of data obtained liom instrumented aircraft is performed. These data were gathered on flights in a mountain wave above the Pyrenees during ALPEX on March 23, 1982. The observed two-and three-dimensional thermal and dynamical structure of the flow is presented. Beneath 7 km altitude. strong three-dimensional response in the atmosphere can be seen in the wind and temperature fields. It appears that the response is almost two-dimensional above this height. Rather pronounced lee waves
doi:10.3402/tellusa.v38i1.11704
fatcat:sjfo74m7hfdiddfsu242pja7ei