sjöbrisfronten
A sjöbrisfront, often translated as sea breeze front, is a meteorological phenomenon occurring along coastlines. It is characterized by a boundary between the cooler, moist air originating from the sea and the warmer, drier air from the land. This temperature and moisture difference creates a localized zone of convergence.
The development of a sjöbrisfront is driven by differential heating. During the day, land heats up faster
As the sjöbrisfront moves inland, it can cause a noticeable drop in temperature and an increase in