147,777 research outputs found
The Heston Riemannian distance function
The Heston model is a popular stock price model with stochastic volatility
that has found numerous applications in practice. In the present paper, we
study the Riemannian distance function associated with the Heston model and
obtain explicit formulas for this function using geometrical and analytical
methods. Geometrical approach is based on the study of the Heston geodesics,
while the analytical approach exploits the links between the Heston distance
function and the sub-Riemannian distance function in the Grushin plane. For the
Grushin plane, we establish an explicit formula for the Legendre-Fenchel
transform of the limiting cumulant generating function and prove a partial
large deviation principle that is true only inside a special set
Nonstationary Stochastic Simulation of Strong Ground-Motion Time Histories : Application to the Japanese Database
For earthquake-resistant design, engineering seismologists employ
time-history analysis for nonlinear simulations. The nonstationary stochastic
method previously developed by Pousse et al. (2006) has been updated. This
method has the advantage of being both simple, fast and taking into account the
basic concepts of seismology (Brune's source, realistic time envelope function,
nonstationarity and ground-motion variability). Time-domain simulations are
derived from the signal spectrogram and depend on few ground-motion parameters:
Arias intensity, significant relative duration and central frequency. These
indicators are obtained from empirical attenuation equations that relate them
to the magnitude of the event, the source-receiver distance, and the site
conditions. We improve the nonstationary stochastic method by using new
functional forms (new surface rock dataset, analysis of both intra-event and
inter-event residuals, consideration of the scaling relations and VS30), by
assessing the central frequency with S-transform and by better considering the
stress drop variability.Comment: 10 pages; 15th World Conference on Earthquake Engineering, Lisbon :
Portugal (2012
Bayes and maximum likelihood for -Wasserstein deconvolution of Laplace mixtures
We consider the problem of recovering a distribution function on the real
line from observations additively contaminated with errors following the
standard Laplace distribution. Assuming that the latent distribution is
completely unknown leads to a nonparametric deconvolution problem. We begin by
studying the rates of convergence relative to the -norm and the Hellinger
metric for the direct problem of estimating the sampling density, which is a
mixture of Laplace densities with a possibly unbounded set of locations: the
rate of convergence for the Bayes' density estimator corresponding to a
Dirichlet process prior over the space of all mixing distributions on the real
line matches, up to a logarithmic factor, with the rate
for the maximum likelihood estimator. Then, appealing to an inversion
inequality translating the -norm and the Hellinger distance between
general kernel mixtures, with a kernel density having polynomially decaying
Fourier transform, into any -Wasserstein distance, , between the
corresponding mixing distributions, provided their Laplace transforms are
finite in some neighborhood of zero, we derive the rates of convergence in the
-Wasserstein metric for the Bayes' and maximum likelihood estimators of
the mixing distribution. Merging in the -Wasserstein distance between
Bayes and maximum likelihood follows as a by-product, along with an assessment
on the stochastic order of the discrepancy between the two estimation
procedures
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