← RETURN TO SUN
ORBONIX · SUN STRUCTURE

CONVECTIVE ZONE

The outer interior layer of the Sun where hot plasma rises, cools near the surface, and sinks again in a continuous cycle.
↑
↑
↑
↑
↑
↑
CONVECTIVE ZONE
≈ 70–100%
SOLAR RADIUS
≈ 2,000,000 → 5,800 K
TEMPERATURE DECREASE
PLASMA
MAIN MATERIAL
CONVECTION
ENERGY TRANSPORT
HOT → UP
RISING PLASMA
COOL → DOWN
SINKING PLASMA

WHAT IS THE CONVECTIVE ZONE?

The convective zone is the outer region of the Sun's interior, extending from roughly 70% of the Sun's radius all the way to the visible surface. Here, the plasma becomes sufficiently opaque that radiation alone is no longer an efficient way to transport energy. Instead, energy is carried by large-scale motions of the plasma. Hot plasma rises toward the surface. As it loses energy, it becomes cooler and denser and eventually sinks again. This creates enormous convection currents that continuously transport energy outward.
THE CONVECTION CYCLE
01
HEATING
Energy from deeper layers heats the surrounding plasma.
02
RISING
Hot plasma becomes less dense and rises toward the surface.
03
COOLING & SINKING
Near the surface the plasma loses energy, becomes denser and sinks.
CORE
RADIATIVE ZONE
CONVECTIVE ZONE
PHOTOSPHERE
DID YOU KNOW?
The convection cells visible at the Sun's surface can be enormous — some can reach thousands of kilometres across.