The flow()
function uses a raster representing elevation to compute other rasters representing:
Flow accumulation;
Direction of flow;
Watershed basins;
Flooded areas; and/or
Topographic convergence (log of flow accumulation divided by local slope).
More details about the computations can be found at the help page for the GRASS module r.terraflow
] (see grassHelp("r.terraflow")
)
Usage
# S4 method for class 'GRaster'
flow(
x,
direction = "multi",
return = "accumulation",
dirThreshold = Inf,
scratchDir = NULL
)
Arguments
- x
A
GRaster
with a single layer, typically representing elevation.- direction
Character: Either
"single"
or"multi"
. This indicates whether a single-direction flow or multi-direction flow model is used. The default is"multi"
. Partial matching is used and case is ignored.- return
Character vector: Indicates what rasters to return. Partial matching is used and case is ignored. Options include:
"accumulation"
(default): Flow accumulation raster."basins"
: Watershed basins"direction"
: Flow direction"flooded"
: Flooded areas"TCI"
: Topographic convergence index"*"
: All of the above
- dirThreshold
Numeric (default is
Inf
): For the multi-direction flow model, this indicates the amount of accumulated flow above which the single-direction flow rule is used to locate the egress of water from a cell. This is thed8cut
parameter inr.stream.extract
.- scratchDir
Character or
NULL
(default): Directory in which to store temporary files. The GRASS moduler.terraflow
makes a lot of temporary files. If this isNULL
, then a temporary folder in the user's working directory will be used (seegetwd()
).
See also
flowPath()
, streams()
, the GRASS module r.terraflow
(see grassHelp("r.terraflow")
)