Earthquake data analysis of the seismicity of Italy in the period 1/1/1900 – 25/02/2022 for events with magnitude larger than 5.
Author: Matteo Censi
INGV provides data on earthquakes that occurred throughout national territory. We have extracted data of 135 earthquakes of magnitude larger than 5.
| Descriptive statistic | |
|---|---|
| Characteristic | Value |
| Total amount of data | 135 |
| Frequency (Total data/Time period) | 1.10 |
| Years | 123 |
| First data | 01 january 1900 |
| Last data | 25 february 2022 |
| Maximum | 7.0 |
| Minimum | 5.0 |
| Position ranking | |
| Mean | 5.49 |
| Minimum | 5.0 |
| First quartile Q1 | 5.2 |
| Median | 5.4 |
| Third quartile Q3 | 5.7 |
| Maximum | 7.0 |
| Dispersion percentages | |
| Range Q3-Q1 | 0.5 |
| Range (max-min) | 2.0 |
| Standard deviation | 0.45 |
| Variance | 0.20 |
| Relative variability | 0.08 |
The resulting earthquake distribution is investigated in relation to time (periodicities).
Fig 2.1. Time distribution of seismicity (M 5+) from 1900.
Fig 2.2. Number of events (M 5+) every 10 years.
The probability mass function (PMF) for the Poisson distribution is:
where k is the number of occurrences, r is the average rate at which events occur, and t is the time interval. So can we forecast earthquakes using Poisson distribution?
First we need to find the rate (r) of the event 135 events in 1465 months (from 1/1/1900 to 25/02/2022). r = 135/1465 ~0.0922 Second we need to find out the probability that an earthquake doesn't occur in a month (t = 1 ; k = 0) and subtract it from 1 p(0)=0.911968188 ; 1-p=0.088031812 ; so it's 8.8%
How about in 12 months? (t = 12 ; k = 0) p(0)=0.330945342 ; 1-p=0.669054658 ; it's 66.9%
Although this way of forecasting has widely been used, it is quite questionable that these probabilities are trustworthy. Why? There are 2 big assumption behind the Poisson Distribution:
The first assumption is not that true: some earthquakes occur in the same fault line, so they are related to each other. The second assumption is not true: the probability of occurrence of an earthquake is not necessarily constant.
[1] E. Guidoboni, G. Ferrari, D. Mariotti, A. Comastri, G. Tarabusi, G. Sgattoni, G. Valensise (2018) - CFTI5Med, Catalogo dei Forti Terremoti in Italia (461 a.C.-1997) e nell’area Mediterranea (760 a.C.-1500). Istituto Nazionale di Geofisica e Vulcanologia (INGV). http://storing.ingv.it/cfti/cfti5/ [2] INGV - Istituto Nazionale di Geofisica e Vulcanologia http://terremoti.ingv.it/