Interpolate FLYS3 water levels for given stations
Source:R/waterLevelFlys3InterpolateX.R
waterLevelFlys3InterpolateX.Rd
Function to interpolate
FLYS3
water levels for selected stations and return it with the structure of
df.flys
.
Usage
waterLevelFlys3InterpolateX(
river = c("Elbe", "Rhine"),
station = NULL,
station_int = NULL
)
Arguments
- river
a required argument to fill the WaterLevelDataFrame-slot
river
. It has to be typecharacter
, has to have a length of one and can be either Elbe or Rhine.- station
an optional argument to hand over the stationing along the specified
river
. If specified, it has to be typenumeric
and has to have the same length as other optional arguments (id
,station_int
andw
) forming thedata.frame
-component of a WaterLevelDataFrame. If both stationing arguments (station
andstation_int
) are specified, all elements ofstation
have to be equal toas.numeric(station_int / 1000)
. Minimum and maximum allowed values ofstation
areriver
-specific: Elbe (km 0 - 585.7), Rhine (km 336.2 - 865.7).- station_int
an optional argument to hand over the stationing along the specified
river
. If specified, it has to be typeinteger
and has to have the same length as other optional arguments (id
,station
andw
) forming thedata.frame
-component of a WaterLevelDataFrame. If both stationing arguments (station
andstation_int
) are specified, all elements ofstation_int
have to be equal toas.integer(station * 1000)
. Minimum and maximum allowed values ofstation_int
areriver
-specific: Elbe (m 0 - 585700), Rhine (m 336200 - 865700).
Value
An object of class data.frame
with the structure of
df.flys
.
Details
df.flys
contains 1d water level data computed
with SOBEK for every second hectometer (every 200 m). This function
provides a way to interpolate the 30 stationary water levels for selected
stations inbetween these hectometers and returns them with the
data.frame
-structure of the original dataset.
References
Busch N, Hammer M (2009). “Einheitliche Grundlage für die Festlegung der Bemessungswasserspiegellagen der Elbe auf der frei fließenden Strecke in Deutschland.” doi:10.5675/bfg-1650 .
HKV Hydrokontor (2014). “Erstellung eines SOBEK-River Modells für den Rhein von Iffezheim bis Pannerdense Kop als Weiterentwicklung bestehender SOBEK-RE Modelle.”
DELTARES (2018). “SOBEK.” https://download.deltares.nl/en/sobek/.