Solar Spicules: How the Corona Gets Its Heat express

Original: "Energy and mass transport associated with impulsive spicular flows in solar coronal holes"
arXiv:2602.19953 · 2026-02-23 · CC BY 4.0 · 1 min
Short plasma jets at the Sun's surface heat the corona and feed the solar wind.

The Sun's surface boils like water in a pot. Hot gas rises, cools, and sinks: that's convection. Magnetic fields churn around, tearing and reconnecting. In this frenzy, spicules are born: narrow plasma jets that shoot thousands of kilometers upward. They live only a few minutes, but they manage to transfer energy to the Sun's outer atmosphere.

A spicule is a column of gas 200–500 kilometers wide and as tall as Earth's diameter. It appears every 300 seconds, like clockwork.

Spicules don't just shoot up: they push waves and shock fronts ahead of them. These waves compress the gas and heat it. That's how energy from the surface reaches the corona — the tenuous outer layer that is hundreds of times hotter than the surface itself. Without spicules, the corona would cool, and the solar wind in coronal holes would dry up.

Coronal holes are regions where magnetic field lines open into space. From there, the solar wind escapes particularly fast.

So one little jet after another, like a pump, drives heat into the corona. Spicules are not just a pretty sight at the Sun's limb. They are the key to a puzzle that has stumped astrophysicists for 80 years: why the corona is hotter than the surface.

The temperature of the Sun's corona is about a million degrees, while the surface is only 5500 degrees. That's like the air around a campfire being hotter than the flame itself.

Scientists
Ludwig BoltzmannEnrico FermiCecilia Payne-GaposchkinJoseph von FraunhoferFred Lawrence WhippleGalileo Galilei
Concepts
solar corona coronal heating mechanism black hole corona core Solar wind plasma heating chromosphere mercury wind stress ocean-atmosphere coupling tropical cyclone heat transport black hole accretion winds hot jupiter atmospheres coronal mass ejection sea surface temperature space weather Ocean heat content convection marine heatwave