At 2 km above the atmosphere, the temperature for a parcel of dry air is 10 ooC and pressure is 800 hPa. What is the potential temperature of this air parcel? Cpp of air 1.005 kJ/kgK and ideal gas constant of air is 0.287 kJ/kgK 290 K 296 K 302 K 308 k
Question
At 2 km above the atmosphere, the temperature for a parcel of dry air is 10 ooC and pressure is 800 hPa. What is the potential temperature of this air parcel? Cpp of air 1.005 kJ/kgK and ideal gas constant of air is 0.287 kJ/kgK 290 K 296 K 302 K 308 k
Solution
The potential temperature is the temperature that a parcel of air would have if it were brought adiabatically (i.e., without exchange of heat or mass) to a standard reference pressure, typically 1000 hPa (hectopascals). The formula to calculate the potential temperature (θ) is:
θ = T * (1000/P)^(R/Cp)
where:
- T is the actual temperature in Kelvin
- P is the actual pressure in hPa
- R is the ideal gas constant for air (0.287 kJ/kgK)
- Cp is the specific heat capacity of air at constant pressure (1.005 kJ/kgK)
First, convert the given temperature from Celsius to Kelvin. The conversion formula is T(K) = T(C) + 273.15. So, T = 10°C + 273.15 = 283.15 K.
Then, substitute the known values into the potential temperature formula:
θ = 283.15 * (1000/800)^(0.287/1.005)
Solving the equation gives the potential temperature θ ≈ 290 K. So, the potential temperature of the air parcel is approximately 290 K.
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