Interpolates the ground points and creates a rasterized digital terrain model. The algorithm uses the points classified as "ground" and "water" (Classification = 2 and 9, respectively, according to LAS file format specifications) to compute the interpolation. How well the edges of the dataset are interpolated depends on the interpolation method used. A buffer around the region of interest is always recommended to avoid edge effects.
grid_terrain(
las,
res = 1,
algorithm,
...,
keep_lowest = FALSE,
full_raster = FALSE,
use_class = c(2L, 9L),
Wdegenerated = TRUE,
is_concave = FALSE
)
An object of class LAS or LAScatalog.
numeric. The resolution of the output Raster
. Can optionally be a RasterLayer
.
In that case the RasterLayer
is used as the layout.
Unused
logical. This option forces the original lowest ground point of each cell (if it exists) to be chosen instead of the interpolated values.
logical. By default the interpolation is made only within the convex hull of the point cloud. This prevents meaningless interpolations where there is no data. If TRUE, each pixel of the raster is interpolated.
integer vector. By default the terrain is computed by using ground points (class 2) and water points (class 9).
logical. The function always checks and removes degenerated ground points for computing the DTM to avoid unexpected behaviours, such as infinite elevation. If TRUE, a warning is thrown to alert users to the presence of degenerated ground points.
boolean. By default the function tries to compute a DTM that
has the same shape as the point cloud by interpolating only in the convex
hull of the points. If the point cloud is concave this may lead to weird values
where there are no points. Use is_concave = TRUE
to use a concave hull.
This is more computationally -involved and requires the concaveman package.
A RasterLayer
containing a numeric value in each cell. If the RasterLayer
s
are written on disk when running the function with a LAScatalog
, a virtual raster mosaic is
returned (see gdalbuildvrt)
This section appears in each function that supports a LAScatalog as input.
In lidR
when the input of a function is a LAScatalog the
function uses the LAScatalog processing engine. The user can modify the engine options using
the available options. A careful reading of the
engine documentation is recommended before processing LAScatalogs
. Each
lidR
function should come with a section that documents the supported engine options.
The LAScatalog
engine supports .lax
files that significantly improve the computation
speed of spatial queries using a spatial index. Users should really take advantage a .lax
files,
but this is not mandatory.
Supported processing options for a LAScatalog
in grid_*
functions (in bold). For
more details see the LAScatalog engine documentation:
chunk size: How much data is loaded at once. The chunk size may be slightly modified internally to ensure a strict continuous wall-to-wall output even when chunk size is equal to 0 (processing by file).
chunk buffer: This function guarantees a strict continuous wall-to-wall output. The
buffer
option is not considered.
chunk alignment: Align the processed chunks. The alignment may be slightly modified internally to ensure a strict continuous wall-to-wall output.
progress: Displays a progress estimate.
output files: Return the output in R or write each cluster's output in a file.
Supported templates are {XLEFT}
, {XRIGHT}
, {YBOTTOM}
, {YTOP}
,
{XCENTER}
, {YCENTER}
{ID}
and, if chunk size is equal to 0 (processing
by file), {ORIGINALFILENAME}
.
select: The function 'knows' what should be loaded and this option is not considered.
filter: Read only the points of interest.
# NOT RUN {
LASfile <- system.file("extdata", "Topography.laz", package="lidR")
las = readLAS(LASfile, filter = "-inside 273450 5274350 273550 5274450")
#plot(las)
dtm1 = grid_terrain(las, algorithm = knnidw(k = 6L, p = 2))
dtm2 = grid_terrain(las, algorithm = tin())
# }
# NOT RUN {
dtm3 = grid_terrain(las, algorithm = kriging(k = 10L))
plot(dtm1)
plot(dtm2)
plot(dtm3)
plot_dtm3d(dtm1)
plot_dtm3d(dtm2)
plot_dtm3d(dtm3)
# }
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