It masses increases and the weight increases
A stationary front occurs when two air masses meet but don't move. It can result in prolonged periods of cloudy, rainy weather.
The temperature and density of the air masses. the air masses moves when hot air and cold air gets together
The water is evaporated from the ocean to form clouds. The air mass that contains the water moves around and the clouds go with them. When air moves from a high pressure to a low pressure zone, that's how wind works.
When cold air moves in and meets warm moist air, it creates a temperature contrast that can lead to the formation of clouds, precipitation, and potentially severe weather such as thunderstorms or snowstorms. This meeting of air masses is known as a front, and the interaction between the two air masses can result in changes in weather conditions.
A stationary front is when warm and cold air masses meet but neither advances. Weather along a stationary front can include prolonged periods of rain, as warm air rises over the cool air and forms clouds. Temperature and precipitation can vary along the front, leading to a mix of weather conditions.
Continental polar
Weather is caused by the interaction of air,water,and sun. This forms air masses which can soon form fronts where air moves from high pressure areas to low pressure areas.
In an anticyclone, air moves in a clockwise direction in the Northern Hemisphere and counterclockwise in the Southern Hemisphere, diverging outward from a high-pressure center. This results in generally settled weather conditions with clear skies and light winds. Anticyclones typically bring dry and stable weather due to the sinking motion of air masses within them.
Weather travels because the wind pushes it slowly to other states, like hurricanes travel very quickly because they spin so fast but rain moves slower because rain clouds are heavy and full so it takes a while for the wind to push it that far!!!
Air masses move due to differences in temperature, pressure, and moisture levels between regions. These differences create pressure gradients that drive the movement of air masses from high pressure to low pressure areas. Other factors such as the rotation of the Earth and the presence of large-scale weather systems also influence the movement of air masses.
As an air mass moves away from its source region into a new region, it brings its particular weather conditions, moisture and temperature, to areas over which it travels. At the same time, its characteristic properties are slowly modified by exposure to new environments.