Function to compute flood extent or flood duration SpatRaster
along the German federal waterways Elbe and Rhine using the 1d water level algorithm hyd1d::waterLevelFlood2()
Source: R/flood2.R
flood2.Rd
Computes flood extent, if length(seq)
equals 1, or flood
duration for the active floodplains along the German federal waterways Elbe
and Rhine based on 1d water levels computed by
waterLevelFlood2
provided by package hyd1d in
analogy to the INFORM 3 module 'Flut2'.
Arguments
- x
has to by type
SpatRaster
and has to include both input layerscsa
(cross section areas) anddem
(digital elevation model). To compute water levels along the River Elbe,x
has to be in the coordinate reference system ETRS 1989 UTM 33N, for the River Rhine in ETRS 1989 UTM 32N. Other coordinate reference systems are not permitted.- seq
has to be type
c("POSIXct", "POSIXt")
orDate
and have a length larger than 0. Values ofseq
must be in the temporal range between 1960-01-01 and yesterday (Sys.Date() - 1
). InternallywaterLevelFlood2()
usesgetGaugingDataW
to obtain daily water level information fromdf.gauging_data
.- filename
supplies an optional output filename and has to be type
character
.- ...
additional arguments as for
writeRaster
.
Details
For every time step provided in seq
, flood2()
computes
a 1d water level using waterLevelFlood2
along the
requested river section. This 1d water level is transfered to a wl
(water level) raster layer, which is in fact a copy of the csa
(cross section areas) layer, and then compared to the dem
(digital elevation model) layer. Where the wl
layer is
higher than the dem
, layer flood duration is increased by 1.
Examples
# \donttest{
options("hydflood.datadir" = tempdir())
library(hydflood)
# import the raster data and create a raster stack
c <- st_crs("EPSG:25833")
e <- ext(309000, 310000, 5749000, 5750000)
x <- hydSpatRaster(ext = e, crs = c)
# create a temporal sequence
seq <- seq(as.Date("2016-12-01"), as.Date("2016-12-31"), by = "day")
# compute a flood duration
fd <- flood2(x = x, seq = seq)
# }