How is fog created by the Labrador Current and the Gulf Stream?

Fog is created when the cold Labrador Current meets the warmer waters of the Gulf Stream along the eastern coast of North America. As the warm, moist air from the Gulf Stream rises over the colder air from the Labrador Current, it cools and condenses, forming fog. This phenomenon is particularly common in regions like the Grand Banks of Newfoundland, where the temperature contrast is significant. The resulting fog can be thick and persistent, impacting maritime navigation in the area.