How a calm flow turns itself into a storm express

Original: "Unstable magnetic reconnection self-generates turbulence"
arXiv:2602.21422 · 2026-02-24 · CC BY 4.0 · 1 min
Magnetic fields in cosmic plasma can twist a calm flow into turbulent chaos all by themselves.

A calm river suddenly starts churning in the middle of a flat stretch: that's the puzzle the authors of a new study set out to solve. They took a thin layer of charged gas with a very weak magnetic field and tracked on a computer what would happen to it. At first, everything flows smoothly, like water from a tap. Then, in one spot, the layer thins out, and the magnetic field lines, which previously lay parallel, begin to snap and reconnect.

This reconnection is like a rubber band in a tangle of yarn snapping, its ends whipping in opposite directions. Each such snap injects a bit of chaos into the flow. At first the chaos is weak, but the snaps repeat, and soon the whole flow is boiling: vortices appear, eddies, tiny jets. And no one pushed the flow: it stirred itself up.

The main source of energy is not the breaks themselves, but how the vortices interact with the large-scale magnetic field. Small magnetic fluctuations hand off energy to the ordinary motion of the gas, and this cascade does not die out.

This matters for understanding the cosmos. The solar wind, plasma jets from the vicinity of black holes, comet tails — all of them are turbulent. Previously, scientists thought turbulence came from outside. Now we see it can be born from within, out of a smooth flow, thanks to magnetic reconnection.

The solar wind at Earth travels at about 400 kilometers per second—20 times faster than a bullet. And nearly all of that flow is turbulent: vortices constantly form and vanish, ranging in size from hundreds of meters to thousands of kilometers.

Scientists
Hendrik LorentzShuji NakamuraVera RubinRobert HookeJohann Jakob BalmerErwin Schrödinger
Concepts
magnetic reconnection turbulence magnetic energy turbulent mixing frustrated magnet turbulent coagulation wind stress permanent magnet instability turbine resonant frequency anomalous hall effect Kelvin-Helmholtz instability energy cascade quantum magnetism earthquake Faraday's law of electromagnetic induction current sheet eddy magnetorotational supernova