VLF/LF subionospheric propagation anomalies
Access restrictednot evaluatedHypothesis, stated so it could fail
Amplitude or phase of very-low-frequency transmitter signals received over a path crossing an epicentral region changes measurably in the days before a large earthquake.
What the evidence actually shows
Reported in retrospective case studies, chiefly from a small number of groups. Prospective tests with pre-registered thresholds are scarce, and the reported effects have not been reproduced independently at a rate that would support operational use.
Confounds that must be excluded first
Solar-terrestrial activity, transmitter maintenance, seasonal and diurnal propagation changes, and receiver drift all move these signals. Any of them can produce an "anomaly" in a record inspected after an earthquake is already known about.
- Data required
- Continuous VLF/LF receiver time series along fixed transmitter-receiver paths
- Candidate sources
- Research receiver networks; no open global archive located