Leggi la politica sulla privacy per maggiori informazioni sui cookies. Facendo clic su "Accetto", autorizzi l'uso dei cookies non essenziali.
This enchanting weather event is
particularly notable when temperatures exceed 15 degrees Celsius,
signaling the revival of one of the area's most fascinating natural
spectacles.
Caligo occurs as a result of a unique interaction between the atmosphere
and the Mediterranean Sea. When a flow of warmer air moves over the
surface of the sea, which maintains cooler temperatures of approximately
13-14 degrees Celsius, a striking transformation begins.
The warmer
air, laden with moisture, encounters the cooler seawater, leading to a
process of evaporation. This interaction is crucial, as it generates an
abundance of water vapor that is essential for the formation of fog.
As the warm, moist air rises and cools, it reaches the dew point, the
critical temperature at which air must be cooled at constant pressure
for condensation to occur.
At this juncture, the water vapor condenses
rapidly, resulting in the formation of countless tiny vapor droplets.
These droplets coalesce to create a thick, ethereal fog that blankets
the landscape, shrouding the picturesque coastal villages and dramatic
cliffs of the Cinque Terre in a mystical veil.