The wind generated by this air movement is known as a katabatic wind.
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The area is also known for the Bora, a type of katabatic wind.
From the en.wikipedia.org
A katabatic wind originates from radiational cooling of air atop a plateau, a mountain, glacier, or even a hill.
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This is known a katabatic wind or mountain breeze.
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If the slopes are covered with ice and snow, the katabatic wind will blow during the day, carrying the cold dense air into the warmer, barren valleys.
From the en.wikipedia.org
Adiabatic heating also occurs in the Earth's atmosphere when an air mass descends, for example, in a katabatic wind or Foehn or chinook wind flowing downhill over a mountain range.