sjöbrisfront
A sjöbrisfront, often translated as sea breeze front, is a meteorological phenomenon occurring along coastlines. It is essentially a shallow, cool air boundary that forms when warm inland air rises and is replaced by cooler, denser air from the sea. This influx of cooler air moves inland, creating a distinct front.
The formation of a sjöbrisfront is driven by differential heating. During the day, land heats up faster
Sjöbrisfronts are most common on warm, sunny days when the land-sea temperature contrast is significant. They