Temp/Pressure Relationship Open Parcel of Air

In summary, when warming a parcel of air that is open, its pressure will decrease and its density will increase due to the molecules moving further apart. The parcel will continue to expand until its pressure is equal to that of the surrounding air. This is similar to how a hot air balloon works, as it is open at the bottom and the heated air inside expands and becomes less dense, causing it to rise.
  • #1
firefuze
I know that in a closed parcel of air, if we increase temperature then pressure rises and density remains constant

If we warm a parcel of air that is open i.e not enclosed, such as the atmosphere.
What happens to pressure? do we say it increases or decreases?

The book I have states; If the heated air is not contained, its molecules-given greater kinetic energy will move further apart and will expand and its density will decrease. The parcel of heated air will continue to expand until its pressure is equal to that of the surrounding air
 
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  • #2
Hello ff, :welcome:

I agree with the book statement. If you expand it a little: before heating the pressure was also that of the surrounding air. So imho the pressure remains equal.

If you go into this further: the change in density and volume does mean that the force balance on the heated volume of air changes and as a consequence it may want to move upwards.
 
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  • #3
Suppose you have a closed parcel of air in a cylinder with a massless frictionless piston above, and atmospheric air outside. What do you think will happen if you add heat to the parcel of air in the cylinder, in terms of its volume, its pressure, and its density?
 
  • #4
Book answer is good. It's how a hot air balloon works. They are open at the bottom.
 

Related to Temp/Pressure Relationship Open Parcel of Air

1. What is the Temp/Pressure Relationship Open Parcel of Air?

The Temp/Pressure Relationship Open Parcel of Air, also known as the adiabatic process, is a mathematical relationship that describes how temperature and pressure change in an air parcel as it rises or descends in the atmosphere.

2. How does the temperature change in an open parcel of air as it rises?

As an open parcel of air rises, it expands due to the decrease in atmospheric pressure. This expansion causes the air molecules to spread out and decrease in density, leading to a decrease in temperature. This process is known as adiabatic cooling.

3. How does the pressure change in an open parcel of air as it rises?

As an open parcel of air rises, it experiences a decrease in pressure due to the decrease in atmospheric pressure. This decrease in pressure is known as adiabatic expansion. The pressure decreases at a rate of approximately 1 hPa per 30 meters of vertical rise.

4. What is the relationship between temperature and pressure in an open parcel of air?

The relationship between temperature and pressure in an open parcel of air is known as the adiabatic lapse rate. This rate varies depending on the moisture content of the air parcel, but on average, the temperature decreases by approximately 1°C per 100 meters of vertical rise, while the pressure decreases by approximately 1 hPa per 30 meters of vertical rise.

5. How does the Temp/Pressure Relationship Open Parcel of Air affect weather patterns?

The Temp/Pressure Relationship Open Parcel of Air plays a crucial role in weather patterns. As air rises and cools due to adiabatic cooling, it can reach its dew point and form clouds and precipitation. This process also impacts air stability and the formation of weather systems such as thunderstorms and hurricanes.

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