Lably
Skip to content

Chapman function

  • 2 min read
  • 4 chapters

Related on Lably

Through Physical quantity, Angle and Trigonometric functions

The Chapman function is named after Sydney Chapman, who introduced the function in 1931. It has been applied for absorption (esp. optical absorption) and the ionosphere.

Definition

In an isothermal model of the atmosphere, the density ϱ(h) varies exponentially with altitude h according to the Barometric formula:

ϱ(h)=ϱ0exp⁡(−hH),

where ϱ0 denotes the density at sea level (h=0) and H the so-called scale height. The total amount of matter traversed by a vertical ray starting at altitude h towards infinity is given by the integrated density ("column depth")

X0(h)=∫h∞ϱ(l)dl=ϱ0Hexp⁡(−hH).

For inclined rays having a zenith angle z, the integration is not straight-forward due to the non-linear relationship between altitude and path length when considering the curvature of Earth. Here, the integral reads

Xz(h)=ϱ0exp⁡(−hH)∫0∞exp⁡(−1H(s2+l2+2lscos⁡z−s))dl,

where we defined s=h+RE (RE denotes the Earth radius).

The Chapman function ch⁡(x,z) is defined as the ratio between slant depth Xz and vertical column depth X0. Defining x=s/H, it can be written as

ch⁡(x,z)=XzX0=ex∫0∞exp⁡(−x2+u2+2xucos⁡z)du.

Sign in to keep reading

3 more chapters are free with a Lably account.

More in Physics