openquake.hmtk.seismicity.completeness package¶
Submodules¶
openquake.hmtk.seismicity.completeness.base module¶
Module :mod:’openquake.hmtk.seismicity.completeness.base’ defines an abstract base class for :class:’CataloguCompleteness <BaseCatalogueCompleteness>
openquake.hmtk.seismicity.completeness.comp_stepp_1971 module¶
Module :mod: ‘openquake.hmtk.seismicity.completeness.comp_stepp_1972’ defines the openquake.hmtk implementation of the Stepp (1972) algorithm for analysing the completeness of an earthquake catalogue
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class
openquake.hmtk.seismicity.completeness.comp_stepp_1971.
Stepp1971
[source]¶ Bases:
openquake.hmtk.seismicity.completeness.base.BaseCatalogueCompleteness
Implements the completeness analysis methodology of Stepp (1972) Stepp, J. C. (1972) Analysis of Completeness of the Earhquake Sample in the Puget Sound Area and Its Effect on Statistical Estimates of Earthquake Hazard. NOAA Environmental Research Laboratories
The original methodology of J. C. Stepp (1972) implements a graphical method in which the devation of the observed rate from the expected Poisson rate is assessed by judgement. To implement the selection in an automated fashion this implementation uses optimisation of a 2-segment piecewise linear fit to each magnitude bin, using the segment intersection point to identify the completeness period.
Adaptation implemented by Weatherill, G. A., GEM Model Facility, Pavia
Attribute numpy.ndarray magnitude_bin: Edges of the magnitude bins Attribute numpy.ndarray sigma: Sigma lambda defined by Equation 4 in Stepp (1972) Attribute numpy.ndarray time_values: Duration values Attribute numpy.ndarray model_line: Expected Poisson rate for each magnitude bin Attribute numpy.ndarray completeness_table: Resulting completeness table -
completeness
(catalogue, config)[source]¶ Gets the completeness table
Parameters: - catalogue – Earthquake catalogue as instance of :class: openquake.hmtk.seismicity.catalogue.Catalogue
- config (dict) – Configuration parameters of the algorithm, containing the following information: ‘magnitude_bin’ Size of magnitude bin (non-negative float) ‘time_bin’ Size (in dec. years) of the time window (non-negative float) ‘increment_lock’ Boolean to indicate whether to ensure completeness magnitudes always decrease with more recent bins
Returns: 2-column table indicating year of completeness and corresponding magnitude numpy.ndarray
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get_completeness_points
(n_years, sigma, n_mags, n_time)[source]¶ Fits a bilinear model to each sigma-n_years combination in order to get the crossover point. The gradient of the first line must always be 1 / sqrt(T), but it is free for the other lines
Parameters: - n_years (numpy.ndarray) – Duration of each completeness time window
- sigma (numpy.ndarray) – Poisson variances of each time-magnitude combination
- n_mags (int) – Number of magnitude bins
- n_time (int) – Number of time bins
Returns: - comp_time (Completeness duration)
- gradient_2 (Gradient of second slope of piecewise linear fit)
- model_line (Expected Poisson rate for data (only used for plot)
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openquake.hmtk.seismicity.completeness.comp_stepp_1971.
get_bilinear_residuals_stepp
(input_params, xvals, yvals, slope1_fit)[source]¶ Returns the residual sum-of-squares value of a bilinear fit to a data set - with a segment - 1 gradient fixed by an input value (slope_1_fit)
Parameters: - input_params (list) –
- Input parameters for the bilinear model [slope2, crossover_point,
- intercept]
- xvals (numpy.ndarray) – x-values of the data to be fit
- yvals (numpy.ndarray) – y-values of the data to be fit
- slope1_fit (float) – Gradient of the first slope
Returns: Residual sum-of-squares of fit
- input_params (list) –