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Most aurorae occur in a band known as the auroral zone[2][2] which is typically 3° to 6° in latitudinal extent and at all local times or longitudes.
The auroral zone is typically 10° to 20° from the magnetic pole defined by the axis of the Earth's magnetic dipole. During a geomagnetic storm, the auroral zone will expand to lower latitudes. The diffuse aurora is a featureless glow in the sky which may not be visible to the naked eye even on a dark night and defines the extent of the auroral zone.
Most aurorae occur in a band known as the auroral zone[2][2] which is typically 3° to 6° in latitudinal extent and at all local times or longitudes.
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