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Vanda Grubišić and Brian J. Billings

during this time are highly unsteady, showing a transition between wave regimes. At 1200 UTC (cf. Fig. 19e ) 26 March, the wave over Owens Valley weakens as the westerly flow enters the valley, forcing a stronger wave response over and to the lee of the Inyo range. This strong westerly jet appears to detach from the ground at the foot of the Sierra lee slope and extend across the valley. An incipient rotor with surface flow deceleration underneath the lee-wave crest is seen over the valley center

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