The lower the density, the wider-spread the particles are, increasing the movement of the air pollutants released at earth's surface. Low density is caused by increased volume because of increased temperature.
it affects it by when you decide to measure the density the air movement always needs to be in play because if it is not then you will get the wrong answer
Warm air is less dense than cold air meaning warm air is lighter so when they meet it causes less dense air(hot air) to move up causing frontal rain.
Wind. or cold to warm lol
Cold fronts and occluded fronts generally move from west to east, while warm fronts move poleward. Because of the greater density of air in their wake, cold fronts and cold occlusions move faster than warm fronts and warm occlusions. Mountains and warm bodies of water can slow the movement of fronts.[2] When a front becomes stationary, and the density contrast across the frontal boundary vanishes, the front can degenerate into a line which separates regions of differing wind velocity, known as a shearline. This is most common over the open ocean.
Wind is the result of pressure differences. These pressure differences can arise in a number of ways, including at fronts, where air masses meet.
Fronts only occur at the boundary of air masses. The Tropics, however are pretty uniform in their high heat and humidity, so there is little in the way of air mass differences.
There's also occluded fronts and stationary fronts, but they are slightly less important--so yes. Kind of.
Warm air is less dense than cold air meaning warm air is lighter so when they meet it causes less dense air(hot air) to move up causing frontal rain.
Warm air is less dense than cold air meaning warm air is lighter so when they meet it causes less dense air(hot air) to move up causing frontal rain.
The differences between cold fronts and warm fronts is that, cold fronts are hard and nasty while warm fronts are soft and easy to sex :D Unknown ....
Wind. or cold to warm lol
Cold fronts and occluded fronts generally move from west to east, while warm fronts move poleward. Because of the greater density of air in their wake, cold fronts and cold occlusions move faster than warm fronts and warm occlusions. Mountains and warm bodies of water can slow the movement of fronts.[2] When a front becomes stationary, and the density contrast across the frontal boundary vanishes, the front can degenerate into a line which separates regions of differing wind velocity, known as a shearline. This is most common over the open ocean.
Stationary fronts themselves do not influence temperature. However, one side will always be colder than the other, and vice versa.
when 2 air masses combine the colder one is forced under the warmer one because of density differences. there are usually thunderstorms on fronts
The movement of wheather fronts from high pressure (cyclone) to low pressure systems(anticyclone).
true
Wind is the result of pressure differences. These pressure differences can arise in a number of ways, including at fronts, where air masses meet.
Fronts only occur at the boundary of air masses. The Tropics, however are pretty uniform in their high heat and humidity, so there is little in the way of air mass differences.
movement of weather fronts