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Stefano Serafin, Lukas Strauss, and Vanda Grubišić

waves and strong downslope winds is well documented east of the Rocky Mountains in Colorado ( Lilly 1978 ) and in Wyoming ( French et al. 2015 ; Grubišić et al. 2015 ), as well as along the eastern Adriatic coast of the Mediterranean Sea ( Smith 1987 ) and over the ice shelf east of the Antarctic Peninsula ( Elvidge et al. 2015 ). In fact, flow acceleration beneath a large-amplitude mountain wave is the most widely accepted explanation for the onset of strong and potentially damaging downslope

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