We measure electric charge in the atmosphere near sea level to detect anomalies that may indicate upcoming seismic activity at specific regions in the world. Based on long-time observations, a seismic event may occur up to about 9 days from the moment that an anomaly was detected. Estimated regions are marked at a thin line, which is perpendicular to the plane of the ecliptic. The strength of an anomaly is indicated by code yellow, orange or red to mark the seismic potential as moderate, strong or major respectively. Uncertainty remains due to unknown tectonic stress levels.

Atmosphere broadcast channels
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Earthquake broadcast channels
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