The air temperature rises when particles in the air begin to move faster. The energy of the motion of particles is called thermal energy.
When warm moist air rises, it cools, causing the water vapor it contains to condense and form clouds. As the air continues to rise, this condensation can lead to precipitation such as rain, snow, or hail. This process is known as adiabatic cooling and is responsible for the formation of most weather phenomena.
Warm moist air rises because it is less dense than the surrounding cool air. As the warm air rises, it expands and cools, leading to condensation and the formation of clouds and precipitation. This process is known as convection.
Increases
No, clouds form when warm, moist air rises and cools, causing water vapor to condense into water droplets or ice crystals. When air sinks, it typically becomes warmer and drier, which discourages cloud formation.
A tornado's funnel cloud forms when warm, moist air rises rapidly and creates a rotating column of air. This spinning motion causes the air to condense into a funnel shape, which is visible as the iconic tornado funnel cloud.
Condensation occurs when moist air rises because as air ascends, the atmospheric pressure decreases, causing the air to expand and cool. When the air cools, it reaches its dew point temperature, causing water vapor to condense into liquid water droplets, forming clouds.
Condensation may occur when moist air rises because of the different arrangement of water molecules.
Correct.
Condensation occurs when moist air rises because as the air moves higher in the atmosphere, it cools down. When the air cools, it reaches its dew point, which is the temperature at which it can no longer hold all of the water vapor it contains. This excess water vapor then condenses into liquid water droplets, forming clouds or precipitation.
As warm, moist air rises in the atmosphere, it cools and condenses, forming clouds and eventually leading to the possibility of precipitation such as rain or snow.
lapse rate
When warm moist air rises, it cools, causing the water vapor it contains to condense and form clouds. As the air continues to rise, this condensation can lead to precipitation such as rain, snow, or hail. This process is known as adiabatic cooling and is responsible for the formation of most weather phenomena.
Evaporation.
The temperature of air is decreased.
The temperature of air is decreased.
When altitude rises, the air pressure and density both decrease. When temperature rises that means that more air is pushing down on it. So this means that the air pressure and density rise when temperature rises.
When altitude rises, the air pressure and density both decrease. When temperature rises that means that more air is pushing down on it. So this means that the air pressure and density rise when temperature rises.