Sun-Earth Connection
Particles/s
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Deflected
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Geomagnetic idx
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Active CMEs
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How it works

The Sun constantly emits a stream of charged particles — the solar wind. During coronal mass ejections (CMEs), huge plasma bubbles erupt outward; when they reach Earth, the planet's magnetosphere deflects most particles, but strong events cause geomagnetic storms.

Kp ~ log(n_particles * v_wind / B_shield)
F_lorentz = q(v × B)  — deflects charged particles
  • Solar activity — scales the baseline rate of particles leaving the Sun's surface.
  • Solar wind speed — how fast particles travel from Sun to Earth.
  • Trigger CME — launches a coronal mass ejection burst toward Earth's magnetosphere.

Earth's magnetosphere (the pale arc) deflects most incoming particles around the shield, which is also what produces the aurora at the poles.