What Heats the Chromosphere and Corona to High Temperatures?

The Sun generates energy through nuclear fusion deep within its core, which radiates outward to the surface and into the star’s atmosphere. While the Sun’s visible surface, the photosphere, is intensely hot, the temperature of the solar atmosphere dramatically increases with distance from it. This thermal inversion, where the outer layers are millions of degrees hotter than the surface beneath them, defies standard physical expectations and remains a central focus of solar physics research.

The Solar Atmosphere and the Temperature Paradox

The Sun’s atmosphere is composed of distinct layers, establishing the scale of this heat problem. The photosphere, the visible surface, maintains a temperature of approximately 5,800 Kelvin (K). According to thermodynamics, the temperature should steadily drop as energy moves outward from the hotter interior.

Above the photosphere is the chromosphere, where the temperature begins to rise from a low of around 4,400 K to several tens of thousands of degrees. The disparity becomes extreme in the corona, the Sun’s outermost atmospheric layer, which reaches temperatures between one and three million Kelvin. This means the atmosphere is hundreds of times hotter than the surface. This immense temperature boost requires a non-thermal mechanism to transport and deposit vast amounts of energy far from the Sun’s core.

Wave-Based Energy Transfer

One major theoretical framework proposes that mechanical energy generated deep within the Sun’s interior is transported to the corona via waves. The churning motion of plasma in the convection zone generates various types of waves that carry energy along the magnetic field lines into the upper atmosphere.

Alfvén waves are considered the most promising candidates for energy transport. These magneto-hydrodynamic waves involve plasma and magnetic field lines oscillating together, moving energy outward from the photosphere. Observations confirm that these waves possess sufficient energy to heat the corona to the observed temperatures.

Heating occurs when these waves dissipate their energy in the corona. As the waves travel through the thin plasma, they are damped by physical processes like turbulence and wave-particle interactions. This converts the wave’s kinetic energy directly into heat, a process that must happen efficiently and close to the Sun.

Magnetic Reconnection and Nanoflares

A second leading explanation centers on the Sun’s intense magnetic activity. The magnetic field lines are constantly twisted and tangled by the movement of underlying plasma, storing enormous amounts of magnetic energy. This energy can be suddenly released through magnetic reconnection.

Magnetic reconnection occurs when opposing magnetic field lines are forced together, break, and rapidly snap back into a simpler configuration. This explosive rearrangement converts stored magnetic energy into kinetic energy and heat, accelerating the local plasma. These events are similar to solar flares, but occur on a much smaller scale.

Astrophysicist Eugene Parker proposed that the cumulative effect of millions of tiny, frequent magnetic explosions, termed nanoflares, provides the necessary constant heating. Although a single nanoflare releases little energy, their sheer frequency continuously replenishes the corona’s thermal energy. Scientists have found evidence of fast, localized heating events, such as nanojets, which are the expected signature of these magnetic reconnection events.

Current Research and Future Exploration

The question of whether waves, nanoflares, or a combination of both is the dominant heating mechanism remains unresolved. Scientists are using sophisticated space missions to gather data and settle the debate. The NASA Parker Solar Probe (PSP) is designed to fly directly through the solar corona, making close-range measurements of the plasma and magnetic fields.

The European Space Agency’s Solar Orbiter (SolO) works in tandem with PSP, providing remote sensing observations of the Sun’s large-scale coronal structure. By coordinating efforts, the probes can simultaneously measure the heating source and its resulting effects, allowing researchers to estimate the coronal heating rate.

These missions seek signatures confirming the theories, such as the damping rate of Alfvén waves or the thermal fingerprints of nanoflares. Early results indicate that turbulence, tied to the dissipation of both waves and magnetic energy, plays a significant part in the heating process. Further data analysis is expected to provide a definitive answer to this long-standing solar mystery.