Lyman-alpha — where it appears
Named by 2 essays across 2 fields — each of them below, with the objects they name alongside it.
An escape that stops following the starlight
The standard estimate of how fast a planet loses its atmosphere assumes the loss grows in proportion to the ultraviolet light it absorbs. It does, up to a point. Beyond about ten thousand erg per square centimetre per second the escaping gas is fully ionised, its heat leaves as Lyman-α light instead of lifting anything, and the loss grows only as the square root of the flux — so the one efficiency every calculation needs is really a function of where the planet sits.
A wind measured by the wall it piles up
The wind of a star like the Sun is far too thin to see. Its mass-loss rate is about 2 × 10⁻¹⁴ of a solar mass a year, too faint to produce any spectral feature of its own, though it controls how fast the star spins down and what happens to the atmospheres of its planets. The only measurements come from somewhere else: the place, far out, where that wind runs into interstellar gas and stacks hot hydrogen into a wall, which leaves a faint notch in the star's own Lyman-α light.
Named alongside it
The objects these essays reach for when they reach for this one.
AstrosphereAtmospheric escapeCharge exchangeEnergy-limited escapeHeating efficiencyHot jupiterMass lossParker windPhoton-limited escapeRecombination-limited escapeStellar windSub-neptune