International audienceSince the pioneering work of Landwehr et al. (1979), Hosking et al. (1985) and their collaborators, the Probability Weighted Moments (PWM) method has been very popular, simple and efficient to estimate the parameters of the Generalized Extreme Value (GEV) distribution when modeling the distribution of maxima (e.g., annual maxima of precipitations) in the Identically and Independently Distributed (IID) context. When the IID assumption is not satisfied, a flexible alternative, the Maximum Likelihood Estimation (MLE) approach offers an elegant way to handle nonstationarities by letting the GEV parameters to be time dependent. Despite its qualities, the MLE applied to the GEV distribution does not always provide accurate r...
A new method is proposed for modelling the yearly maxima of sub-daily precipitation, with the aim of...
Abstract. Following the work of Azzalini ([2] and [3]) on the skew normal distribution, we propose a...
The perception that hydrometeorological processes are non stationary on timescales that are applicab...
International audienceSince the pioneering work of Landwehr et al. (1979), Hosking et al. (1985) and...
International audienceFor a wide range of applications in hydrology and climate studies, the return ...
The purpose of this study is to compare the Generalized Extreme Value (GEV) parameter estimation by ...
The standard method of the maximum likelihood has poor performance in GEV parameter estimates for sm...
International audienceAnalyzing the behavior of heavy precipitation, high temperatures, and extremes...
The generalised extreme value (GEV) distribution is a three parameter family that describes the asym...
International audienceFollowing the work of Azzalini ([2] and [3]) on the skew normal distribution, ...
Numerous studies show that climatic extremes have increased substantially in the second half of the ...
In this paper, temperature extremes are forecast by employing the block maxima method of the General...
The use of partial probability weighted moments (PPWM) for estimating hydrological extremes is compa...
The generalized Pareto distribution (GPD) is often used in the statistical analysis of climate extre...
In extreme value theory and other related risk analysis fields, probability weighted moments (PWM) h...
A new method is proposed for modelling the yearly maxima of sub-daily precipitation, with the aim of...
Abstract. Following the work of Azzalini ([2] and [3]) on the skew normal distribution, we propose a...
The perception that hydrometeorological processes are non stationary on timescales that are applicab...
International audienceSince the pioneering work of Landwehr et al. (1979), Hosking et al. (1985) and...
International audienceFor a wide range of applications in hydrology and climate studies, the return ...
The purpose of this study is to compare the Generalized Extreme Value (GEV) parameter estimation by ...
The standard method of the maximum likelihood has poor performance in GEV parameter estimates for sm...
International audienceAnalyzing the behavior of heavy precipitation, high temperatures, and extremes...
The generalised extreme value (GEV) distribution is a three parameter family that describes the asym...
International audienceFollowing the work of Azzalini ([2] and [3]) on the skew normal distribution, ...
Numerous studies show that climatic extremes have increased substantially in the second half of the ...
In this paper, temperature extremes are forecast by employing the block maxima method of the General...
The use of partial probability weighted moments (PPWM) for estimating hydrological extremes is compa...
The generalized Pareto distribution (GPD) is often used in the statistical analysis of climate extre...
In extreme value theory and other related risk analysis fields, probability weighted moments (PWM) h...
A new method is proposed for modelling the yearly maxima of sub-daily precipitation, with the aim of...
Abstract. Following the work of Azzalini ([2] and [3]) on the skew normal distribution, we propose a...
The perception that hydrometeorological processes are non stationary on timescales that are applicab...