For --, escape is well described by the dilute high-velocity tail of a nearly hydrostatic exosphere. For --, collisions couple the escaping gas into hydrodynamic atmospheric escape; the intermediate regime requires a kinetic or transonic calculation.
The hydrostatic-tail estimate follows by integrating a Maxwell distribution over outward velocities exceeding escape speed. The Jeans escape flux isThereforeWhen , this is of order the free thermal supply ; quantitatively the flow is hydrodynamic and its conserved mass-loss rate is through the transonic wind.
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