Hydrodynamic escape Created 2026-10-14 Updated 2026-11-05
Hydrodynamic escape is atmospheric loss in which collisions couple the gas into a bulk outward flow. Heating raises the gas pressure and can drive expansion against gravity; an escaping solution often accelerates through a sonic point. The temperature and velocity profiles must satisfy energy and momentum balances, rather than being fixed by a collisionless high-speed tail alone.
The flow can carry heavier species along with the dominant light gas, provided coupling is strong enough. Energy-limited atmospheric escape estimates a mass-loss rate by assigning a fraction of absorbed stellar power to gravitational work. That estimate can fail when radiative cooling, limited heating supply or other parts of the flow's energy budget dominate. A small Jeans escape parameter is suggestive of strong escape, but does not by itself specify a unique outflow.
Three physically distinct mechanisms are as follows.
Thermal-tail escape, a bulk hydrodynamic wind, and nonthermal particle energization are three distinct channels; a detected tail need not distinguish them alone. Jeans escape and hydrodynamic atmospheric escape are both thermal mechanisms in the broad sense, but have different distribution functions and dynamical assumptions.
Comparable hydrostatic thermal escape requires comparable Jeans escape parameter . For the same escaping species and ,
Thus Jupiter at 5 au needs an exobase temperature at least about thirty times Earth's at the same irradiation to have comparable Jeans escape flux.
For the inner planet, the usable EUV power is . If the binding energy per unit escaping mass is , energy-limited atmospheric escape gives
The time to lose a fraction of the planetary mass is therefore
This neglects Roche-lobe reduction, radiative cooling, changes in radius and flux, and the planet's orbital evolution. If the gas is lifted only from , replace in the denominator by .