RegioWeissmanSeas {flood}

Quantile estimation: Weissman's extrapolation for seasonal data

Description

Estimation of the p-quantile based on multiple local Hill estimators and Weissman's extrapolation formula with seasonality. We assume heavy-tail homogeneity within each season, i.e., all local EVI's are the same.

Usage

RegioWeissmanSeas(x, j = 1, p, ...)

Arguments

x

List of 2 elements: each element is consistent a vector or matrix of observations

j

The number of the target site, i.e., if j=2 the p-quantile of the second station is estimated.

p

The probability of interest; should be between 1-k_j/n_j and 1, where n_j is the sample length of the j-th column.

...

additional arguments, see RegioWeissman

Value

Point estimate of seasonal p-quantile of column j and a short description.

Examples

library("evd")
# Local & seasonal (observations of 80 years at one station):
x1 <- rgev(80, 2, 1, 0.2) # observations from season 1
x2 <- rgev(80, 3, 1, 0.3) # observations from season 2
x <- list(x1, x2)
RegioWeissmanSeas(x=x, j=1, p=0.99)

x1 <- matrix(rgev(400, 3, 1, 0.1), ncol=4) # observations of season 1 at 4 stations
x2 <- matrix(rgev(400, 2, 1, 0.3), ncol=4) # observations of season 2 at 4 stations
x <- list(x1, x2)
RegioWeissmanSeas(x=x, j=1, p=0.99)