Description Usage Arguments Details Value Author(s) References Examples
We compute the exceedance probability, that is, the probability that a
specified value c
(a magnitude of a seismic event, a flow level... )
will be exceeded in D
time units.
1 2 3 |
type_kernel |
The kernel function. You can use four types: "e" Epanechnikov, "n" Normal, "b" Biweight and "t" Triweight. The Normal kernel is used by default. |
vec_data |
The data sample (earthquake magnitudes, flow levels, wind speed...) |
c |
The concrete level in which we want to compute the exceedance probability. |
bw |
The bandwidth parameter. The plug-in method of Polansky and Baker (2000) is used by default. |
Dmin |
Minimum value for D time units (years, days... ). Default is Dmin=0. |
Dmax |
Maximum value for D time units (years, days... ). Default is Dmax=15. |
size_grid |
Length of a grid in which we compute the exceedance function. The size is 50 by default. |
lambda |
The mean activity rate. |
The exceedance function is usually calculated assuming that the occurrence process
of events follows a Poisson one. In this case, the exceedance function, that is, the
probability of an specific value c
is calculated as
R(c,D) = 1- exp(-λ D(1-F_h(c)).
See, for example, Orlecka-Sikora (2008) or Quintela del Rio (2010) for earthquake data applications.
Returns a list containing:
Estimated_values |
Vector containing the estimated function. |
grid |
The used grid. |
bw |
Value of the bandwidth. |
Graciela Estevez Perez graci@udc.es and Alejandro Quintela del Rio aquintela@udc.es
Orlecka-Sikora, B. (2008) Resampling methods for evaluating the uncertainty of the nonparametric magnitude distribution estimation in the probabilistic seismic hazard analysis. Tectonophysics 456, 38–51.
Quintela-del-Rio, A. (2010) On non-parametric techniques for area-characteristic seismic hazard parameters. Geophysical Journal International 180, pp. 339–346.
Quintela-del-Rio, A. and Estevez-Perez, G. (2012) Nonparametric Kernel Distribution Function Estimation with kerdiest: An R Package for Bandwidth Choice and Applications, Journal of Statistical Software 50(8), pp. 1-21. URL http://www.jstatsoft.org/v50/i08/.
1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 | # Working with earthquake data. We use the catalogue of the National
# Geographic Institute (IGN) of Spain and select the data of the Northwest
# of the Iberian Peninsula.
data(nwip)
require(chron)
require(date)
# we consider the data with magnitude greater than 3
mg<-nwip$magnitude[nwip$magnitude>3.0]
x1<-nwip$year
x2<-nwip$month
x3<-nwip$day
ys<-paste(x1,x2,x3)
earthquake_date<-as.character(ys)
y1s<-as.date(earthquake_date, order = "ymd")
# we compute the total number of years
y2s<-as.POSIXct(y1s)
z<-years(y2s)
n.years<-length(levels(z))
# the mean rate of earthquakes per year
lambda<-length(mg)/n.years
## Not run:
# we estimate the exceedance probability for a value of the
# the magnitude = 4
est<-ef(vec_data=mg, m_c=4, lambda=lambda)
plot(est$grid, est$Estimated_values, type="l",
xlab="years", ylab="Probability of Exceedance")
## End(Not run)
|
Add the following code to your website.
For more information on customizing the embed code, read Embedding Snippets.