You signed in with another tab or window. Reload to refresh your session.You signed out in another tab or window. Reload to refresh your session.You switched accounts on another tab or window. Reload to refresh your session.Dismiss alert
Peter Powers edited this page Sep 18, 2017
·
3 revisions
TODO need about-deaggregation; check Ex 7 link
What are ε and ε₀?
The ground motion, Y, that might be recorded at a specific site from an earthquake 'source' with a given magnitude and distance is typically modeled as a log-normal variate such that the logarithm of Y, which we denote y, has a normal distribution, with mean, μ, and standard deviation, σ. Epsilon is defined as the standardized y at a site from a specific source: ε = (y – μ) ∕ σ. Because we compute the probability of exceeding some ground motion at a site, p₀, in probabilisitic seismic hazard analysis, our deaggregation tools instead report ε₀ = (y₀ – μ) ∕ σ.