Atkinson Boore 2003 Intensity Model
Class Name
- RAtkinsonBoore2003IntensityModel
Location in Objects Pane
- Models > Model > Hazard > Earthquake > Intensity > Atkinson Boore 2003 Intensity
Model Description
Model Form
- This model produces the spectral acceleration or the peak ground acceleration at specified locations for given magnitude and hypocentre location of several earthquake sources as input, based on the Atkinson-Boore (2003) attenuation relation.
- For more information, see Boore-Atkinson (2003)
DDM Sensitivities
Properties
Object Name
- Name of the object in Rt
- Allowable characters are upper-case and lower-case letters, numbers, and underscore (“_”).
- The name is unique and case-sensitive.
Display Output
- Determines whether the model is allowed to print messages to the Output Pane.
Magnitude List
- Magnitudes of various earthquake sources
Hypocentre Location List
- Hypocenter locations of earthquake sources, which automatically will yield the radius \({R}\) to the various output locations
Epsilon
- \({\varepsilon}\) = Model error, typically a standard normal random variable
Event Type
- Type of the earthquake event that can either be Interface or In-slab.
Response Type
- Type of the response than can either be \({S_a}\) or \({PGA}\).
Smoothness
- “Smoothed” option will smooth the kinks in the model and the “Original” option will use the model as it is.
Period List
- List of the natural periods at which the intensity is evaluated
Structure Location List
- List of the locations where the intensity will be computed at them (the output will give as many intensity values as the locations provided here)
Shear Wave Velocity List
- List of the shear wave velocities at the specified locations
Output
- Earthquake intensities (as many as the locations provided in the input).
- The output is an automatically generated generic response object, which takes the object name of the model plus “Response”.
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References
- Atkinson, G. M., & Boore, D. M. (2003). Empirical ground-motion relations for subduction-zone earthquakes and their application to Cascadia and other regions. Bulletin of the Seismological Society of America, 93(4), 1703–1729