Mountains, like shores, have breezes, too.
A mountain breeze and a valley breeze are two related, localized winds that occur one after the other on a daily cycle. They are not the same as anabatic and katabatic winds, which are larger and stronger. These winds are opposite from each other. Mountain winds blow from mountain towards valley after sunset, when mountain cools down and valley zone is comparatively warmer. While valley breezes occur when the warm air rises up the sides of the valley, warm air in a mountain breeze will rise up the middle.
At night the air in the high quotes is cooled more than the one in the valley and therefore sinks, producing a wind, while in the morning, when the air warms up, an opposite flow is produced. This is common during the warm season. Proximity to the sea, with the water thermal inertia, would probably amplify this effect.
Additionally it might also happen that the passage to the open sea will behave as a venturi for the air forced in/out of the bay when the mountain breeze happens, resulting in regular winds.
If the turbines are optimized for those kind of winds, it can make sense.