Derivation of Adiabatic Lapse Rate

In summary, potential energy is neglected in the derivation of the adiabatic lapse rate because it assumes a vertically stable atmosphere with no change in altitude, and to simplify the energy balance as the air parcel only exchanges heat through compression and expansion. Introducing potential energy would complicate the derivation.
  • #1
pm272
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In the derivation of the adiabatic lapse rate, upon using the 1st law of thermodynamics: Why is potential energy neglected? The parcel of air is doing work PdV which is balanced by the internal energy term, cvdT.

I can't think of a reason to neglect gravitational potential energy here.

Thanks.
 
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  • #2
The gravitational potential energy appears through the pressure P(z) because of the hydrostatic condition.
 
  • #3


Hi there,

The reason for neglecting potential energy in the derivation of the adiabatic lapse rate is because we are assuming a vertically stable atmosphere in which the air parcel is not changing its altitude. In this case, there is no change in potential energy, so it can be neglected in the overall energy balance.

Additionally, the adiabatic lapse rate is derived assuming that the air parcel is only exchanging heat with its surroundings through compression and expansion, not through any other processes. In this scenario, the work done by the air parcel (PdV) is balanced by the change in internal energy (cvdT), as you mentioned.

If we were to consider potential energy in this scenario, it would introduce an additional source of energy exchange and would complicate the derivation of the adiabatic lapse rate. Therefore, for the sake of simplicity and to focus on the main processes at play, potential energy is typically neglected in this context.

I hope this helps to clarify the reasoning behind neglecting potential energy in the derivation. Let me know if you have any further questions or concerns.

 

FAQ: Derivation of Adiabatic Lapse Rate

What is the Adiabatic Lapse Rate?

The Adiabatic Lapse Rate is a measure of the rate at which the temperature of a parcel of air changes as it moves vertically in the atmosphere. It is typically expressed in units of degrees Celsius per kilometer (°C/km) or degrees Fahrenheit per 1000 feet (°F/1000ft).

How is the Adiabatic Lapse Rate calculated?

The Adiabatic Lapse Rate is calculated using the ideal gas law, which relates the pressure, volume, and temperature of a gas. It is also affected by the specific heat capacity of the air and the gravitational acceleration. The resulting formula is -g/cp, where g is the gravitational acceleration and cp is the specific heat capacity of air at constant pressure.

What is the difference between the Dry and Moist Adiabatic Lapse Rates?

The Dry Adiabatic Lapse Rate (DALR) is the rate at which the temperature of a dry parcel of air changes as it moves vertically in the atmosphere. The Moist Adiabatic Lapse Rate (MALR) takes into account the additional cooling effect of water vapor condensing in the parcel as it rises. The MALR is lower than the DALR, typically around 6°C/km compared to 10°C/km for the DALR.

How does the Adiabatic Lapse Rate affect weather patterns?

The Adiabatic Lapse Rate plays a crucial role in determining the stability of the atmosphere and the formation of weather patterns. If the environmental lapse rate (the actual rate at which the temperature changes in the atmosphere) is less than the Adiabatic Lapse Rate, the atmosphere is said to be stable and there is little vertical movement of air. If the environmental lapse rate is greater than the Adiabatic Lapse Rate, the atmosphere is unstable and there is potential for strong vertical movement and the formation of severe weather events.

How does the Adiabatic Lapse Rate vary with altitude?

The Adiabatic Lapse Rate is a constant value that does not change with altitude. However, the actual temperature change in the atmosphere can vary due to factors such as humidity, cloud cover, and topography. In general, the Adiabatic Lapse Rate is more accurate in the lower levels of the atmosphere, but can become less reliable at higher altitudes due to the influence of other factors.

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