Decreases
When a parcel of air is forced downward, atmospheric pressure increases, causing the air to become compressed and therefore the temperature is also raised.
A parcel of air that is less dense than the surrounding air is known as a "buoyant air parcel." This occurs when the temperature of the air parcel is higher than that of the surrounding air, causing it to rise due to its lower density. As it ascends, it may cool and potentially lead to cloud formation if it reaches the condensation level. This process is fundamental to atmospheric convection and weather patterns.
When moist air is heated in an airtight vessel, the temperature of the air increases, causing the water vapor to evaporate more readily, which can lead to an increase in humidity. If there is no way for the water vapor to escape the vessel, it will remain inside as part of the air mixture.
When a parcel of air is less dense than the surrounding air, it will rise due to buoyancy forces. As the parcel rises, it will expand and cool adiabatically, which can lead to cloud formation and possibly precipitation. This process is known as atmospheric convection.
Nothing
Orographic effect
Decreases
An air parcel is an imaginary body of air with the basic properties of atmospheric air.
Lifting Condensation Level is altitude at which clouds begin in a rising parcel of air. Lifting condensation level(LCL) can be said to be the level to which an unsaturated air parcel can be lifted adiabatically before it becomes saturated.Remember,this unsaturated air parcel is moist
It cools and condenses
When a parcel of air is forced downward, atmospheric pressure increases, causing the air to become compressed and therefore the temperature is also raised.
- Moist air has water vapor in it. - As a moist air parcel rises, the water vapor will condense (latent heat of condensation) - latent heat is released, meaning a temperature increase occurs within that air parcel, effectively dampening its lapse rate. Thus, the latent heat of condensation is working to decrease the lapse rate because sensible heat is being released in the process; its called the Moist Adiabatic Rate (MAR) In contrast, the Dry Adiabatic Rate (DAR) considered for Dry air (no water vapor) does not involve condensation, and thus no latent heat is released; meaning the lapse rate is unaffected.
Usually rain showers or thunderstorms result.
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.
As a parcel of air rises, it expands and cools adiabatically. This cooling causes relative humidity to increase, as the air temperature drops and its capacity to hold moisture decreases. If the air parcel reaches its dew point temperature, the relative humidity will reach 100% and condensation or cloud formation may occur.
When a parcel of air is saturated with water vapor the relative humidity of that parcel of air is 100%.