Adiabatic Temperature Change in Rising Air

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SUMMARY

The discussion focuses on deriving the change in temperature with height for a parcel of air that rises adiabatically, using the hydrostatic equation and the ideal gas law. The key equation derived is ##dp = -\rho g dz##, leading to the expression for temperature change as ##-\frac{\gamma-1}{\gamma} \frac{mg}{K_B}##. Participants emphasized the importance of substituting density in terms of pressure and temperature, specifically using ##\rho = \frac{pM}{RT}## to facilitate the derivation. The final relationship established is ##pT^{\frac{\gamma}{(1-\gamma)}}=C##, confirming the connection between pressure and temperature during adiabatic processes.

PREREQUISITES
  • Understanding of the hydrostatic equation and its application in atmospheric science.
  • Familiarity with the ideal gas law and its variables, including pressure, volume, and temperature.
  • Knowledge of adiabatic processes and the concept of specific heat ratios, denoted as ##\gamma##.
  • Basic calculus skills for manipulating differential equations.
NEXT STEPS
  • Study the derivation of the hydrostatic equation in atmospheric thermodynamics.
  • Learn about adiabatic processes and their implications in meteorology.
  • Explore the relationship between pressure, volume, and temperature in ideal gases using the ideal gas law.
  • Investigate the significance of the specific heat ratio ##\gamma## in thermodynamic processes.
USEFUL FOR

This discussion is beneficial for students and professionals in atmospheric science, meteorology, and thermodynamics, particularly those interested in understanding adiabatic processes and their effects on temperature changes in rising air parcels.

Physgeek64
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Homework Statement


The hydrostatic equation expresses the change in pressure dp due to a layer of

atmosphere of thickness dz as

constant volume.

##dp = −\rho g dz ##
Using this expression, show that the change in temperature with height for a parcel of air that rises adiabatically in the atmosphere can be expressed as
##-\frac{\gamma-1}{\gamma} \frac{mg}{K_B}##

Homework Equations

The Attempt at a Solution


So I think we're trying to find ##\frac{\partial T}{\partial z}_S ## as this seems like a reversible process

starting off with ##dU=TdS-pdV##
## \frac{\partial U}{\partial T}_z dT +\frac{\partial U}{\partial z}_T dz = TdS-pdV##
## \frac{3NK_B}{2}\frac{\partial T}{\partial z}_S +\frac{\partial U}{\partial z}_T =-p\frac{\partial V}{\partial z}_S##

The fact that i can't find ## \frac{\partial V}{\partial z}_S## makes me think I've gone wrong somewhere

Many thanks
 
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What is the relation between T and p for an adiabatic reversible expansion? From the ideal gas law, what is the density expressed as a function of the temperature, pressure, and molecular weight?
 
Chestermiller said:
What is the relation between T and p for an adiabatic reversible expansion? From the ideal gas law, what is the density expressed as a function of the temperature, pressure, and molecular weight?

##TV^{\gamma -1} =constant## and ##\rho=\frac{m}{V} ## ?
 
Physgeek64 said:
##TV^{\gamma -1} =constant## and ##\rho=\frac{m}{V} ## ?
I asked for T vs P, not V., $$\rho=\frac{Pm}{RT}$$
 
Chestermiller said:
I asked for T vs P, not V., $$\rho=\frac{Pm}{RT}$$
would there not be a factor of n in there?
 
Physgeek64 said:
would there not be a factor of n in there?
In the equation I wrote, The m is the molecular weight and R is the ideal gas constant. $$\rho=\frac{nm}{V}$$
 
Chestermiller said:
In the equation I wrote, The m is the molecular weight and R is the ideal gas constant. $$\rho=\frac{nm}{V}$$
Oh of course. But i don't see how to use these. Was i on the right track?
 
Physgeek64 said:
Oh of course. But i don't see how to use these. Was i on the right track?
No. Actually, you weren't on the right track. You can start by substituting ##\rho=\frac{pM}{RT}## into the equation $$dp=-\rho g dz$$. Then you substitute the relationship between p and T (in terms of ##\gamma##) for an adiabatic reversible expansion.
 
Chestermiller said:
No. Actually, you weren't on the right track. You can start by substituting ##\rho=\frac{pM}{RT}## into the equation $$dp=-\rho g dz$$. Then you substitute the relationship between p and T (in terms of ##\gamma##) for an adiabatic reversible expansion.

so I get ##dp=-\frac{pmg}{K_BT}dz= -\frac{Nmg}{V}dz##

I can't see where to go from here
 
  • #10
$$pT^{\frac{\gamma}{(1-\gamma)}}=C$$
 
  • #11
Chestermiller said:
$$pT^{\frac{\gamma}{(1-\gamma)}}=C$$
Thank you, I have done it now :)
 

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