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In the potential temperature equation: k is:
Question



In the potential temperature equation:

k is:

A.

Ratio of gas constant to specific heat at constant pressure for ideal diatomic gas

B.

Ratio of gas constant to latent heat at constant pressure of ideal diatomic gas

C.

Ratio of gas constant to Boltzmann constant

D.

Ratio of gas constant to height at which θ\thetaθ is measured

Correct option is A


Understanding the Potential Temperature Equation:
· Potential temperature (θ) is a thermodynamic parameter that represents the temperature an air parcel would have if it were brought adiabatically to a reference pressure P0​.
· It is calculated using the formula

where:
· T is the actual temperature,
· P is the actual pressure,
· P0 is the reference pressure (often 1000 hPa),
· k=R/Cp​.
k Definition:
· k=R/Cp​:
· R is the specific gas constant for air.
· Cp​ is the specific heat at constant pressure.
· This ratio determines how the temperature changes with pressure during adiabatic processes.
· Explanation of Options:
· Option 1: Correct.
· k is defined as the ratio of the gas constant (R) to the specific heat at constant pressure (Cp​) for the gas, which is ideal for air or diatomic gases.
· Option 2: Incorrect.
· k is not related to latent heat. Latent heat governs phase changes, not adiabatic processes.
· Option 3: Incorrect.
· Boltzmann constant (kB​) is not part of this equation.
· Option 4: Incorrect.
· k is not related to height but rather thermodynamic properties.
Thus, the correct answer is Option 1: Ratio of gas constant to specific heat at constant pressure for ideal diatomic gas.
Information Booster: 1. Specific Heat and Gas Constant:
· Cp=Cv+R, where Cv is the specific heat at constant volume.
· For a diatomic gas like air:
· Cp=7/2 R, Cv=5/2R.
2. Adiabatic Processes:
· During adiabatic compression/expansion, the relationship between pressure and temperature is governed by k=R/Cp​.
3. Applications of Potential Temperature:
· Useful in atmospheric science for analyzing vertical stability of the atmosphere.
· Helps identify layers with different thermodynamic properties

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