Science / radio-science

How Radio Waves Measure Worlds

📐 Measuring the Earth
How Radio Waves Measure Worlds
PIA13277 - The 70-metre antenna at Goldstone: the instrument that reads these shifts. NASA/JPL-Caltech.

Question

How do you measure the atmosphere or gravity of a planet millions of kilometres away?

With a radio signal and a stopwatch. A radio wave changes frequency in exact proportion to the motion of its source relative to you - the Doppler shift, Δf/f = v/c. The Deep Space Network tracks deep-space signals with atomic-clock precision, so a spacecraft moving at just 1 m/s shifts an 8.4 GHz signal by about 28 Hz, and the network resolves a fraction of that. When a signal passes behind a planet, the atmosphere it crosses changes the shift in a measurable way - reading that change gives the atmosphere's density, pressure and temperature profile. The same wobble in the signal maps a planet's gravity field as the spacecraft flies over hidden mass concentrations.

The math

Δf/f = v/c. At v = 1 m/s with c = 299,792,458 m/s: Δf/f = 3.34×10⁻⁹, which at an 8.4 GHz downlink is Δf ≈ 28 Hz. At v = 10 km/s the same signal shifts by ≈ 281 kHz - and the DSN resolves a tiny fraction of a hertz.

Why it matters

The same physics is in your phone (a GPS receiver corrects for Doppler before it fixes your position), in the radar gun on the motorway, and in the redshift that shows the universe is expanding. Viking measured Mars's atmosphere this way in 1976 - the radio wave did the measuring, no surface instrument needed.

Sources

  1. Wikipedia - Doppler effect (Δf/f = v/c) [1]
  2. Wikipedia - Deep Space Network (the 'DSN and radio science' section) [2]