Astrophysics & Space

Atmospheric Scale Height Formula

Computes the vertical scale height H over which the barometric atmospheric pressure and gas density decrease by a factor of e (approx. 2.718).

\[ H = \frac{k_B \cdot T}{m_{mol} \cdot g} = \frac{R_{univ} \cdot T}{M_{molar} \cdot g} \implies P(z) = P_0 \cdot e^{-z/H} \]
Plain Text Formula: H = (R_univ * T) / (M_molar * g) ==> P(z) = P0 * exp(-z / H)

๐Ÿ“ Variable Definitions & Parameters

Symbol Variable Name Standard Unit Physical Definition
\[ H \] Scale Height meters (m) or km Vertical altitude increase producing a 1/e drop in pressure
\[ T \] Atmospheric Temperature Kelvin (K) Mean kinetic gas temperature
\[ M_{molar} \] Mean Molecular Mass kg/mol Mean molecular weight of air (Earth ~0.02897 kg/mol)
\[ g \] Surface Gravity m/sยฒ Gravitational acceleration (Earth 9.81 m/sยฒ)
\[ R_{univ} \] Universal Gas Constant 8.314 J/(molยทK) Molar gas constant

๐Ÿ’ก Worked Engineering Example

Problem Statement:

Calculate Earth's scale height at T = 288 K (M_molar = 0.02897 kg/mol, g = 9.81 m/sยฒ).

Step-by-Step Solution:

  1. Numerator: 8.314 * 288 = 2,394.43
  2. Denominator: 0.02897 * 9.81 = 0.2842
  3. H = 2,394.43 / 0.2842 = 8,425 meters โ‰ˆ 8.43 km
๐ŸŽฏ Result: Earth's atmospheric scale height is approximately 8.43 kilometers.
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