Labrador Current
The dense fogs off Newfoundland occur when warm, moist air from the Gulf Stream blows over the LABRADOR CURRENT
fog
Rainshadow
It is the Gulf Stream
Warm air is less dense then cold air. But moist air is actually less dense than dry air because water vapor has a lower molecular weight than the oxygen and nitrogen that make up most of the atmosphere.
The AIR is very dense, and moist today.
Because more moist air to the south
The source would the ocean. The condensation nuclei would be tiny particles of salt. The advection fog of Newfoundland is formed when warm air (from above the warm Gulf Stream) comes into contact with The Labrador Current (a cold ocean current) near the Grand Banks off of Newfoundland.
No they only have to be connected to the blood stream and the nerve system.
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.
Moist wind is a type of wind that contains a high amount of water vapor or moisture. It is often associated with weather systems that bring precipitation, such as rainstorms or humid conditions. Moist winds can contribute to the formation of clouds and can influence local weather patterns.
Convection Currents