Similar winds occur at other gaps in mountain ranges, such as the tehuantepecer and the jochwinde, and in long channels, such as the Strait of Juan de Fuca between the Olympic Mountains of Washington and Vancouver Island, British Columbia, Hinlopen Strait near Spitsbergen.
Another example is the Koshava wind in Serbia that blows along the Danube River.
[1] The South Carpathian Mountains and Balkan Mountains are channelling the flow into the Danube River basin in Romania and the exiting jet at the Iron Gates is known as the Koshava wind.
[2] More generally, corridor winds affect the local climate of a region (south of France), as well as vegetation.
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