The dense fogs off Newfoundland occur when warm, moist air from the Gulf Stream blows over the LABRADOR CURRENT
Labrador Current
The fast dense current of air is called the jet stream. It flows west to east, dividing cold Arctic air from warmer southern air in the northern hemisphere, influencing weather patterns and the movement of storms.
When dense,cold air meets less dense,warmer air, the warm air is pushed up
When dense,cold air meets less dense,warmer air, the warm air is pushed up
a sea breeze is when land warms up faster than the water so the cooler more dense air above the water rushes in to replace the warmer less dense air above the land.It staarts when the air blows from sea to land
the air is warmer because the sun's rays hit the equater more directly and because it is warmer it becomes more dense
Warmer things are less dense, so as the molasses gets warmer, it becomes less dense or more "liquidy."
No, cold air pushes up warmer air because the warmer air is less dense.
When dense,cold air meets less dense,warmer air, the warm air is pushed up
As air becomes warmer it becomes less dense (as long as the pressure remains constant)
The heat from condensation makes the rising air warmer and stay less dense than the air around it.
the warm air is pushed down because its lees dense than the cold air if cold air is more dense.