4. Determine the height of the water column (precipitation level) precipitated by the air stream in 3 hours, assuming a homogeneous rainfall between points M1 and M2.
Given constants:
Moist air is streaming adiabatically across a mountain range as indicated in the figure.
Equal atmospheric pressures of 100kPa are measured at meteorological stations M0 and M3 and a pressure of 70kPa at station M2. The temperature of the air at M0 is 20∘C.
As the air is ascending, cloud formation sets in at 84.5kPa.
Consider a quantity of moist air ascending the mountain with a mass of 2000kg over each square meter. This moist air reaches the mountain ridge (station M2 ) after 1500 seconds. During that rise an amount of 2.45g of water per kilogram of air is precipitated as rain.
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Hints and Data
The atmosphere is to be dealt with as an ideal gas. Influences of the water vapour on the specific heat capacity and the atmospheric density are to be neglected; the same applies to the temperature dependence of the specific latent heat of vaporisation. The temperatures are to be determined to an accuracy of 1K, the height of the cloud ceiling to an accuracy of 10m and the precipitation level to an accuracy of 1mm.
Specific heat capacity of the atmosphere in the pertaining temperature range:
cp=1005J⋅kg−1⋅K−1
Atmospheric density for p0 and T0 at station M0:ρ0=1.189kg⋅m−3
Specific latent heat of vaporisation of the water within the volume of the cloud:
Lv=2500kJ⋅kg−1cvcp=χ=1.4 and g=9.81m⋅s−2
Context question:
1. Determine temperature T1 at M1 where the cloud ceiling forms.
Context answer:
279
Context question:
2. What is the height h1( at M1) above station M0 of the cloud ceiling assuming a linear decrease of atmospheric density?
Context answer:
1410
Context question:
3. What temperature T2 is measured at the ridge of the mountain range?
Context answer:
271