To optimize magnitude estimation for the earthquake early warning system around the Tehran region, different amplitude‐ and frequency‐based parameters, that is, predominant period (), characteristic period ( τ c ), log‐average period ( τ log ), and peak displacement ( P d ) were analyzed in this article. All parameters were calculated directly from seismic records, with an epicentral distance less than 150 km, and within the initial 3 s of the P waves. The analysis of earthquakes in the 2.4 M L P d and τ c were underestimated, and there was no scaling relationship with the τ log parameter. When combined with the global observations from Japan, Taiwan, and Italy, the results of P d and τ c for the Tehran region produced optimized results.
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Nazeri et al. (2017) studied this question.
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