In a turbulent collapsing cloud, ambipolar drift becomes chaotic and antiphased above and below the midplane, but the region-averaged true mass-to-flux ratio still increases monotonically, while observed values do not match it.
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Ambipolar diffusion and the mass-to-flux ratio in a turbulent collapsing cloud
In a turbulent collapsing cloud, ambipolar drift becomes chaotic and antiphased above and below the midplane, but the region-averaged true mass-to-flux ratio still increases monotonically, while observed values do not match it.