tyearsS {lfstat} | R Documentation |
Calculate Low-Flow Quantiles for given Return Periods
Description
Fits an extreme value distribution using L-moments to the dry spells of a time series of discharges and subsequently estimates quantiles (the so called T-years event) for given return periods. In the presence of zero flow observations a mixed distribution is fitted.
Usage
tyearsS(lfobj, event = 1/probs, probs = 0.01, pooling = NULL,
dist = "wei", check = TRUE, zeta = NULL,
plot = TRUE, col = 1, log = TRUE, legend = TRUE,
rp.axis = "bottom", rp.lab = "Return period", freq.axis = TRUE,
freq.lab = expression(paste("Frequency " *(italic(F)),
" = Non-Exceedance Probability P ",
(italic(X) <= italic(x)))),
xlab = expression("Reduced variate, " * -log(-log(italic(F)))),
ylab = "Quantile",
variable = c("volume", "duration"), aggr = "max",
hyearstart = hyear_start(lfobj), ...)
Arguments
lfobj |
An object of class |
event |
numeric vector specifying the return periods. E.g. |
probs |
Alternate way to specify the return period of the event. |
pooling |
a pooling function, see |
dist |
A character vector of distributions to fit. Basically all distributions provided by Hosking's |
check |
logical, should |
zeta |
numeric vector of length one for manually setting a lower bound. Only a few distributions allow for a lower bound, namely |
plot |
logical. If |
col |
numeric or character vector of length one or as long as |
log |
logical. If |
legend |
logical, should a legend be added to the plot? |
rp.axis |
vector of length one, specifying if and how an additional scale bar for the return periods is drawn. Possible choices are |
rp.lab |
character vector, text above the scale bar for return periods |
freq.axis |
logical, should an additional abscissa showing the probabilities be drawn on top of the plot? |
freq.lab |
character vector, text above the probability axis |
xlab |
character vector, a label for the x axis |
ylab |
character vector, a label for the y axis |
variable |
character vector of length one. Either |
aggr |
function like |
hyearstart |
vector of length one, providing the start of the hydrological year. This is evaluated by |
... |
arguments passed on to |
Details
This function is vectorised over dist
and event
.
According to paragraph 7.4.2 of the WNO manual, special care has to be taken in the presence of zero flow observations. A cdf called G(x) is fitted to the non-zero values of the original time series
If a distribution is fitted which allows for finite lower bound (zeta
), and zeta
is estimated being negative, estimation is repeated constraining zeta = 0
. If this behavior is not desired, the parameter zeta
has to be set explicitly.
Value
An object of class 'evfit'
, see evfit
.
Author(s)
Gregor Laaha
References
Gustard, A. & Demuth, S. (2009) (Eds) Manual on Low-flow Estimation and Prediction. Operational Hydrology Report No. 50, WNO-No. 1029, 136p.
See Also
There are methods for printing summarizing objects of class 'evfit'
.
Examples
data("ngaruroro")
rp <- c(1.3, 3, 5, 35)
sumD <- tyearsS(ngaruroro, event = rp, dist = "wei",
variable = "d", aggr = sum)
sumD
summary(sumD)