Put and . The polytropic stellar wind equations become . At a regular sonic point both derivatives vanish. Matching their minima allows the two positive- branches to join with finite slope; unequal minima either leave a forbidden radial interval or separate the subsonic and supersonic branches. This reduces a singular differential-equation crossing to a geometric minimum comparison.
A stellar wind carries matter away from a star, altering its mass, angular momentum and surroundings. Hot coronal gas can escape through pressure-driven expansion; radiation transfers momentum to gas through continuum or spectral line absorption, or to dust that then drags gas. A magnetic field can transfer rotational energy and angular momentum to an outflow. These mechanisms need not give the same terminal speed or mass loss rate.
For a steady spherical pressure-driven model, conservation of mass gives . Combining the radial Euler equation with an isothermal equation of state gives the Parker wind equation
A smooth transonic branch passes through at , connecting a subsonic inner atmosphere to an escaping supersonic wind. The isothermal Parker wind requires continuing heat input as the gas expands; a polytropic stellar wind instead tracks a changing temperature and must satisfy its own terminal-energy condition. A subsonic isothermal breeze generally tends to a nonzero external pressure, so outward velocity alone does not select the escaping solution.
Figure 1.
Transonic isothermal Parker wind and a pressure-confined breeze
. Details.
The solar wind supplies a nearby example of an outward plasma flow carrying a magnetic field. Profiles of spectral lines, especially absorption shifted by the Doppler effect together with emission, diagnose more distant stellar winds. The critical-point condition and boundary heating constrain ; it is not determined by an escape-speed estimate alone.
For steady spherical polytropic flow, write and use the polytropic equation of state , with . Mass conservation and radial Euler momentum equation are
The mass equation gives . Substitute it into momentum balance to obtain
At a sonic point the derivative coefficient vanishes. A smooth finite-slope solution must make the numerator vanish there too:
Finally . Integrating momentum gives the Bernoulli equation
This is kinetic energy plus specific enthalpy plus gravitational potential per unit mass. The polytropic stellar wind selects a particular transonic branch of these equations.