| 摘要 |
The disclosed earthquake vapor theory, statistically significant in practice, overcomes two difficulties: the dependency on cold weather to pinpoint an earthquake epicenter and the time window not being short enough for evacuation. Finding a vapor nozzle based on boiling temperature can solve the former. Isolating the nozzle to find the next peak of daily maximum after vapor eruption can solve the latter by narrowing the time window to 1-2 days. The embodiments may also be utilized to prevent mysterious air and sea accidents. |
