The image presents a derivation of some formulae used in meteorology, specifically related to the characteristic gas equation, pressure and height relationship, and adiabatic relations. It shows how pressure changes with height and temperature, and how these relationships are derived. We are asked to derive the equation for the height interval between two pressure levels p1 and p2, assuming constant temperature, based on the given equations.

Applied MathematicsPhysicsMeteorologyCalculusIntegrationGas LawsDifferential EquationsLogarithms
2025/4/13

1. Problem Description

The image presents a derivation of some formulae used in meteorology, specifically related to the characteristic gas equation, pressure and height relationship, and adiabatic relations. It shows how pressure changes with height and temperature, and how these relationships are derived. We are asked to derive the equation for the height interval between two pressure levels p1 and p2, assuming constant temperature, based on the given equations.

2. Solution Steps

First, let's identify the relevant equations.
The characteristic gas equation is given as:
pv=RTpv = RT (1)
Where pp is pressure, vv is volume, RR is a gas constant and TT is absolute temperature.
Also,
p=ρRTp = \rho R T (2)
Where ρ\rho is density.
We are given that
gρdz=dpg\rho dz = -dp (A)
And, eliminating the density ρ\rho by means of equation (2), we obtain:
dz=RTgpdpdz = -\frac{RT}{gp} dp (3)
The height interval between two pressure levels p1p_1 and p2p_2 is obtained by integrating equation (3). Since the temperature is constant, we can write:
z1z2dz=p1p2RTgpdp\int_{z_1}^{z_2} dz = -\int_{p_1}^{p_2} \frac{RT}{gp} dp
h2h1=RTgp1p21pdph_2 - h_1 = -\frac{RT}{g} \int_{p_1}^{p_2} \frac{1}{p} dp
Where h1=z1h_1 = z_1 and h2=z2h_2 = z_2
The integral of 1p\frac{1}{p} with respect to pp is ln(p)ln(p):
h2h1=RTg[ln(p)]p1p2h_2 - h_1 = -\frac{RT}{g} [ln(p)]_{p_1}^{p_2}
h2h1=RTg(ln(p2)ln(p1))h_2 - h_1 = -\frac{RT}{g} (ln(p_2) - ln(p_1))
h2h1=RTg(ln(p1)ln(p2))h_2 - h_1 = \frac{RT}{g} (ln(p_1) - ln(p_2))
h2h1=RTgln(p1p2)h_2 - h_1 = \frac{RT}{g} ln(\frac{p_1}{p_2})
If we are using units such that R/g is again 96, while if the logarithms are changed from base e to base 10, the conversion factor 2.303 must be introduced. This gives
h2h1=221.1T(logp1logp2)h_2 - h_1 = 221.1 T(log p_1 - log p_2) feet
[h2h1]=67.47T(logp1logp2)[h_2 - h_1] = 67.47 T(log p_1 - log p_2) metres.

3. Final Answer

The height interval is given by:
h2h1=RTgln(p1p2)h_2 - h_1 = \frac{RT}{g} ln(\frac{p_1}{p_2})
Or,
h2h1=221.1T(logp1logp2)h_2 - h_1 = 221.1 T(log p_1 - log p_2) feet
[h2h1]=67.47T(logp1logp2)[h_2 - h_1] = 67.47 T(log p_1 - log p_2) metres

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