Title: | Calculate Slopes of Roads, Rivers and Trajectories |
---|---|
Description: | Functions and example data to support research into the slope (also known as longitudinal gradient or steepness) of linear geographic entities such as roads <doi:10.1038/s41597-019-0147-x> and rivers <doi:10.1016/j.jhydrol.2018.06.066>. The package was initially developed to calculate the steepness of street segments but can be used to calculate steepness of any linear feature that can be represented as LINESTRING geometries in the 'sf' class system. The package takes two main types of input data for slope calculation: vector geographic objects representing linear features, and raster geographic objects with elevation values (which can be downloaded using functionality in the package) representing a continuous terrain surface. Where no raster object is provided the package attempts to download elevation data using the 'ceramic' package. |
Authors: | Robin Lovelace [aut, cre] , Rosa Félix [aut] , Joey Talbot [aut] , Dan Olner [rev] (Dan reviewed the package for rOpenSci, see https://github.com/ropensci/software-review/issues/420#issuecomment-857662657), Andy Teucher [rev] (Andy reviewed the package for rOpenSci, see https://github.com/ropensci/software-review/issues/420#issuecomment-858231647) |
Maintainer: | Robin Lovelace <[email protected]> |
License: | GPL-3 |
Version: | 1.0.1 |
Built: | 2024-12-06 05:58:44 UTC |
Source: | https://github.com/ropensci/slopes |
Road segments representing suggested route to cycle in Leeds, UK.
cyclestreets_route
cyclestreets_route
An object of class sf
with 18 rows and 14 columns on route
characteristics. See https://rpackage.cyclestreets.net/reference/journey.html
for details.
Simple feature collection with 30 features and 32 fields
See data-raw/cyclestreets_route.R
in the package's github repo for details.
CycleStreets.net
library(sf) class(cyclestreets_route) plot(cyclestreets_route$geometry) cyclestreets_route
library(sf) class(cyclestreets_route) plot(cyclestreets_route$geometry) cyclestreets_route
A dataset containing elevation in and around Lisbon with a geographic resolution of 10m. The dataset is 200 pixels wide by 133 pixels high, covering 2.7 square kilometres of central Lisbon.
dem_lisbon_raster
dem_lisbon_raster
A raster dataset containing elevation above sea level in a 1km bounding box in Lisbon, Portugal.
The dataset was acquired by Instituto Superior Técnico (University of Lisbon) in 2012, covers all the Northern Metropolitan Area of Lisbon, and has a 10m cell resolution, when projected at the official Portuguese EPSG: 3763 - TM06/ETRS89. The dataset was released as an open access dataset with permission from the University of Lisbon to support this project.
https://github.com/rspatial/terra/issues/29
library(sf) library(raster) dim(dem_lisbon_raster) res(dem_lisbon_raster) names(dem_lisbon_raster) plot(dem_lisbon_raster) plot(lisbon_road_network["Avg_Slope"], add = TRUE)
library(sf) library(raster) dim(dem_lisbon_raster) res(dem_lisbon_raster) names(dem_lisbon_raster) plot(dem_lisbon_raster) plot(lisbon_road_network["Avg_Slope"], add = TRUE)
Take a linestring and add a third (z) dimension to its coordinates
elevation_add( routes, dem = NULL, method = "bilinear", terra = has_terra() && methods::is(dem, "SpatRaster") )
elevation_add( routes, dem = NULL, method = "bilinear", terra = has_terra() && methods::is(dem, "SpatRaster") )
routes |
Routes, the gradients of which are to be calculated.
The object must be of class |
dem |
Raster overlapping with |
method |
The method of estimating elevation at points,
passed to the |
terra |
Should the |
An sf object that is identical to the input routes
, except that
the coordinate values in the ouput has a third z
dimension representing
the elevation of each vertex that defines a linear feature such as a road.
library(sf) routes = lisbon_road_network[204, ] dem = dem_lisbon_raster (r3d = elevation_add(routes, dem)) library(sf) st_z_range(routes) st_z_range(r3d) plot(st_coordinates(r3d)[, 3]) plot_slope(r3d) # Get elevation data (requires internet connection and API key): r3d_get = elevation_add(cyclestreets_route) plot_slope(r3d_get)
library(sf) routes = lisbon_road_network[204, ] dem = dem_lisbon_raster (r3d = elevation_add(routes, dem)) library(sf) st_z_range(routes) st_z_range(r3d) plot(st_coordinates(r3d)[, 3]) plot_slope(r3d) # Get elevation data (requires internet connection and API key): r3d_get = elevation_add(cyclestreets_route) plot_slope(r3d_get)
This function takes a series of points located in geographical space
and a digital elevation model as inputs and returns a vector of
elevation estimates associated with each point.
The function takes locations
represented as a matrix of XY (or longitude latitude) coordinates
and a digital elevation model (DEM) with class raster
or terra
.
It returns a vector of values representing estimates of elevation
associated with each of the points.
elevation_extract( m, dem, method = "bilinear", terra = has_terra() && methods::is(dem, "SpatRaster") )
elevation_extract( m, dem, method = "bilinear", terra = has_terra() && methods::is(dem, "SpatRaster") )
m |
Matrix containing coordinates and elevations or an sf object representing a linear feature. |
dem |
Raster overlapping with |
method |
The method of estimating elevation at points,
passed to the |
terra |
Should the |
By default, the elevations are estimated using
bilinear interpolation
(method = "bilinear"
)
which calculates point height based on proximity to the centroids of
surrounding cells.
The value of the method
argument is passed to the method
argument in
raster::extract()
or
terra::extract()
depending on the class of the input raster dataset.
See Kidner et al. (1999) for descriptions of alternative elevation interpolation and extrapolation algorithms.
A vector of elevation values.
Kidner, David, Mark Dorey, and Derek Smith. "What’s the point? Interpolation and extrapolation with a regular grid DEM." Fourth International Conference on GeoComputation, Fredericksburg, VA, USA. 1999.
dem = dem_lisbon_raster elevation_extract(lisbon_road_network[1, ], dem) m = sf::st_coordinates(lisbon_road_network[1, ]) elevation_extract(m, dem) elevation_extract(m, dem, method = "simple") # Test with terra (requires internet connection): if(slopes:::has_terra()) { et = terra::rast(dem_lisbon_raster) elevation_extract(m, et) }
dem = dem_lisbon_raster elevation_extract(lisbon_road_network[1, ], dem) m = sf::st_coordinates(lisbon_road_network[1, ]) elevation_extract(m, dem) elevation_extract(m, dem, method = "simple") # Test with terra (requires internet connection): if(slopes:::has_terra()) { et = terra::rast(dem_lisbon_raster) elevation_extract(m, et) }
elevation_get()
uses the
cc_elevation()
function from the ceramic
package to get
DEM data in raster format anywhere worldwide.
It requires an API that can be added by following guidance in the package's
README
and in the
slopes
vignette.
elevation_get(routes, ..., output_format = "raster")
elevation_get(routes, ..., output_format = "raster")
routes |
Routes, the gradients of which are to be calculated.
The object must be of class |
... |
Options passed to |
output_format |
What format to return the data in?
Accepts |
Note: if you use the cc_elevation()
function directly to get DEM data,
you can cache the data, as described in the package's
README.
A raster object with cell values representing elevations in the
bounding box of the input routes
object.
# Time-consuming examples that require an internet connection and API key: library(sf) library(raster) routes = cyclestreets_route e = elevation_get(routes) class(e) crs(e) e plot(e) plot(st_geometry(routes), add = TRUE)
# Time-consuming examples that require an internet connection and API key: library(sf) library(raster) routes = cyclestreets_route e = elevation_get(routes) class(e) crs(e) e plot(e) plot(st_geometry(routes), add = TRUE)
A dataset representing road segments in Lisbon, with X, Y and Z (elevation) dimensions for each coordinate.
lisbon_road_network
lisbon_road_network
An object of class sf
, key variables of which include
ID of the object
The minimum elevation on the linear feature from ArcMAP
The max elevation on the linear feature from ArcMAP
The mean elevation on the linear feature from ArcMAP
The minimum slope on the linear feature from ArcMAP
The max slope on the linear feature from ArcMAP
The mean slope on the linear feature from ArcMAP
The geometry defining the LINESTRING component of the segment
The dataset covers 32 km of roads in central Lisbon, overlapping with the
area covered by the dem_lisbon_raster
dataset.
Produced by ESRI's 3D Analyst extension
library(sf) names(lisbon_road_network) sum(st_length(lisbon_road_network)) plot(lisbon_road_network["Avg_Slope"])
library(sf) names(lisbon_road_network) sum(st_length(lisbon_road_network)) plot(lisbon_road_network["Avg_Slope"])
A single road segment and a 3d version. Different versions of this dataset are provided.
lisbon_road_segment
lisbon_road_segment
An object of class sf
The lisbon_road_segment
has 23 columns and 1 row.
The lisbon_road_segment_xyz_mapbox
was created with:
lisbon_road_segment_xyz_mapbox = elevation_add(lisbon_road_segment)
.
Produced by ESRI's 3D Analyst extension
lisbon_road_segment lisbon_road_segment_3d lisbon_road_segment_xyz_mapbox
lisbon_road_segment lisbon_road_segment_3d lisbon_road_segment_xyz_mapbox
A route representing a trip from the Santa Catarina area in the East of central Lisbon the map to the Castelo de São Jorge in the West of central Lisbon.
lisbon_route
lisbon_route
An object of class sf
Different versions of this dataset are provided.
The lisbon_route
object has 1 row and 4 columns: geometry, ID,
length and whether or not a path was found.
The lisbon_route_xyz_mapbox
was created with:
lisbon_route_xyz_mapbox = elevation_add(lisbon_route)
.
See the lisbon_route.R
script in data-raw
lisbon_route lisbon_route_3d lisbon_route_xyz_mapbox
lisbon_route lisbon_route_3d lisbon_route_xyz_mapbox
A dataset representing road segments in the Magnolia area of Seattle with X, Y and Z (elevation) dimensions for each coordinate.
magnolia_xy
magnolia_xy
An object of class sf
Accessed in early 2021 from the seattle-streets
layer from the
data-seattlecitygis
website.
names(magnolia_xy) plot(magnolia_xy["SLOPE_PCT"])
names(magnolia_xy) plot(magnolia_xy["SLOPE_PCT"])
Plot a digital elevation profile based on xyz data
plot_dz( d, z, fill = TRUE, horiz = FALSE, pal = colorspace::diverging_hcl, ..., legend_position = "top", col = "black", cex = 0.9, bg = grDevices::rgb(1, 1, 1, 0.8), title = "Slope colors (percentage gradient)", brks = NULL, seq_brks = NULL, ncol = 4 )
plot_dz( d, z, fill = TRUE, horiz = FALSE, pal = colorspace::diverging_hcl, ..., legend_position = "top", col = "black", cex = 0.9, bg = grDevices::rgb(1, 1, 1, 0.8), title = "Slope colors (percentage gradient)", brks = NULL, seq_brks = NULL, ncol = 4 )
d |
Cumulative distance |
z |
Elevations at points across a linestring |
fill |
Should the profile be filled? |
horiz |
Should the legend be horizontal ( |
pal |
Color palette to use, |
... |
Additional parameters to pass to legend |
legend_position |
The legend position. One of "bottomright", "bottom", "bottomleft", "left", "topleft", "top" (the default), "topright", "right" and "center". |
col |
Line colour, black by default |
cex |
Legend size, 0.9 by default |
bg |
Legend background colour, |
title |
Title of the legend, |
brks |
Breaks in colour palette to show.
|
seq_brks |
Sequence of breaks to show in legend. Includes negative numbers and omits zero by default |
ncol |
Number of columns in legend, 4 by default. |
A plot showing the elevation profile associated with a linestring.
library(sf) route_xyz = lisbon_road_segment_3d m = st_coordinates(route_xyz) d = cumsum(sequential_dist(m, lonlat = FALSE)) d = c(0, d) z = m[, 3] slopes:::plot_dz(d, z, brks = c(3, 6, 10, 20, 40, 100))
library(sf) route_xyz = lisbon_road_segment_3d m = st_coordinates(route_xyz) d = cumsum(sequential_dist(m, lonlat = FALSE)) d = c(0, d) z = m[, 3] slopes:::plot_dz(d, z, brks = c(3, 6, 10, 20, 40, 100))
Plot slope data for a 3d linestring with base R graphics
plot_slope( route_xyz, lonlat = sf::st_is_longlat(route_xyz), fill = TRUE, horiz = FALSE, pal = colorspace::diverging_hcl, legend_position = "top", col = "black", cex = 0.9, bg = grDevices::rgb(1, 1, 1, 0.8), title = "Slope colors (percentage gradient)", brks = c(3, 6, 10, 20, 40, 100), seq_brks = seq(from = 3, to = length(brks) * 2 - 2), ncol = 4, ... )
plot_slope( route_xyz, lonlat = sf::st_is_longlat(route_xyz), fill = TRUE, horiz = FALSE, pal = colorspace::diverging_hcl, legend_position = "top", col = "black", cex = 0.9, bg = grDevices::rgb(1, 1, 1, 0.8), title = "Slope colors (percentage gradient)", brks = c(3, 6, 10, 20, 40, 100), seq_brks = seq(from = 3, to = length(brks) * 2 - 2), ncol = 4, ... )
route_xyz |
An sf linestring with x, y and z coordinates, representing a route or other linear object. |
lonlat |
Are the routes provided in longitude/latitude coordinates?
By default, value is from the CRS of the routes ( |
fill |
Should the profile be filled? |
horiz |
Should the legend be horizontal ( |
pal |
Color palette to use, |
legend_position |
The legend position. One of "bottomright", "bottom", "bottomleft", "left", "topleft", "top" (the default), "topright", "right" and "center". |
col |
Line colour, black by default |
cex |
Legend size, 0.9 by default |
bg |
Legend background colour, |
title |
Title of the legend, |
brks |
Breaks in colour palette to show.
|
seq_brks |
Sequence of breaks to show in legend. Includes negative numbers and omits zero by default |
ncol |
Number of columns in legend, 4 by default. |
... |
Additional parameters to pass to legend |
A plot showing the elevation profile associated with a linestring.
plot_slope(lisbon_route_3d) route_xyz = lisbon_road_segment_3d plot_slope(route_xyz) plot_slope(route_xyz, brks = c(1, 2, 4, 8, 16, 30)) plot_slope(route_xyz, s = 5:8)
plot_slope(lisbon_route_3d) route_xyz = lisbon_road_segment_3d plot_slope(route_xyz) plot_slope(route_xyz, brks = c(1, 2, 4, 8, 16, 30)) plot_slope(route_xyz, s = 5:8)
Set lonlat
to FALSE
if you have projected data, e.g. with coordinates
representing distance in meters, not degrees. Lonlat coodinates are assumed
(lonlat = TRUE
is the default).
sequential_dist(m, lonlat = TRUE)
sequential_dist(m, lonlat = TRUE)
m |
Matrix containing coordinates and elevations. The matrix should have three columns: x, y, and z, in that order. Typically these correspond to location in the West-East, South-North, and vertical elevation axes respectively. In data with geographic coordinates, Z values are assumed to be in metres. In data with projected coordinates, Z values are assumed to have the same units as the X and Y coordinates. |
lonlat |
Are the coordinates in lon/lat (geographic) coordinates? TRUE by default. |
A vector of distance values in meters if lonlat = TRUE
or the map units of the input data if lonlat = FALSE
between
consecutive vertices.
x = c(0, 2, 3, 4, 5, 9) y = c(0, 0, 0, 0, 0, 1) m = cbind(x, y) d = sequential_dist(m, lonlat = FALSE) d nrow(m) length(d)
x = c(0, 2, 3, 4, 5, 9) y = c(0, 0, 0, 0, 0, 1) m = cbind(x, y) d = sequential_dist(m, lonlat = FALSE) d nrow(m) length(d)
Calculate the gradient of line segments from a 3D matrix of coordinates
slope_matrix(m, elevations = m[, 3], lonlat = TRUE) slope_matrix_mean(m, elevations = m[, 3], lonlat = TRUE, directed = FALSE) slope_matrix_weighted(m, elevations = m[, 3], lonlat = TRUE, directed = FALSE)
slope_matrix(m, elevations = m[, 3], lonlat = TRUE) slope_matrix_mean(m, elevations = m[, 3], lonlat = TRUE, directed = FALSE) slope_matrix_weighted(m, elevations = m[, 3], lonlat = TRUE, directed = FALSE)
m |
Matrix containing coordinates and elevations. The matrix should have three columns: x, y, and z, in that order. Typically these correspond to location in the West-East, South-North, and vertical elevation axes respectively. In data with geographic coordinates, Z values are assumed to be in metres. In data with projected coordinates, Z values are assumed to have the same units as the X and Y coordinates. |
elevations |
Elevations in same units as x (assumed to be metres).
Default value: |
lonlat |
Are the coordinates in lon/lat (geographic) coordinates? TRUE by default. |
directed |
Should the value be directed? |
A vector of slope gradients associated with each linear element
(each line between consecutive vertices) associated with linear features.
Returned values for slope_matrix_mean()
and
slope_matrix_weighted()
are summary statistics for all
linear elements in the linestring.
The output value is a proportion representing the change in elevation
for a given change in horizontal movement along the linestring.
0.02, for example, represents a low gradient of 2% while 0.08 represents
a steep gradient of 8%.
x = c(0, 2, 3, 4, 5, 9) y = c(0, 0, 0, 0, 0, 9) z = c(1, 2, 2, 4, 3, 0) / 10 m = cbind(x, y, z) slope_matrix_weighted(m, lonlat = FALSE) slope_matrix_weighted(m, lonlat = FALSE, directed = TRUE) # 0 value returned if no change in elevation: slope_matrix_weighted(m,lonlat = FALSE, directed = TRUE, elevations = c(1, 2, 2, 4, 3, 1)) slope_matrix_mean(m, lonlat = FALSE) slope_matrix_mean(m, lonlat = FALSE, directed = TRUE) plot(x, z, ylim = c(-0.5, 0.5), type = "l") (gx = slope_vector(x, z)) (gxy = slope_matrix(m, lonlat = FALSE)) abline(h = 0, lty = 2) points(x[-length(x)], gx, col = "red") points(x[-length(x)], gxy, col = "blue") title("Distance (in x coordinates) elevation profile", sub = "Points show calculated gradients of subsequent lines")
x = c(0, 2, 3, 4, 5, 9) y = c(0, 0, 0, 0, 0, 9) z = c(1, 2, 2, 4, 3, 0) / 10 m = cbind(x, y, z) slope_matrix_weighted(m, lonlat = FALSE) slope_matrix_weighted(m, lonlat = FALSE, directed = TRUE) # 0 value returned if no change in elevation: slope_matrix_weighted(m,lonlat = FALSE, directed = TRUE, elevations = c(1, 2, 2, 4, 3, 1)) slope_matrix_mean(m, lonlat = FALSE) slope_matrix_mean(m, lonlat = FALSE, directed = TRUE) plot(x, z, ylim = c(-0.5, 0.5), type = "l") (gx = slope_vector(x, z)) (gxy = slope_matrix(m, lonlat = FALSE)) abline(h = 0, lty = 2) points(x[-length(x)], gx, col = "red") points(x[-length(x)], gxy, col = "blue") title("Distance (in x coordinates) elevation profile", sub = "Points show calculated gradients of subsequent lines")
This function takes an sf
representing routes over geographical space
and a raster dataset representing the terrain as inputs.
It returns the average gradient of each route feature.
slope_raster( routes, dem, lonlat = sf::st_is_longlat(routes), method = "bilinear", fun = slope_matrix_weighted, terra = has_terra() && methods::is(dem, "SpatRaster"), directed = FALSE )
slope_raster( routes, dem, lonlat = sf::st_is_longlat(routes), method = "bilinear", fun = slope_matrix_weighted, terra = has_terra() && methods::is(dem, "SpatRaster"), directed = FALSE )
routes |
Routes, the gradients of which are to be calculated.
The object must be of class |
dem |
Raster overlapping with |
lonlat |
Are the routes provided in longitude/latitude coordinates?
By default, value is from the CRS of the routes ( |
method |
The method of estimating elevation at points,
passed to the |
fun |
The slope function to calculate per route,
|
terra |
Should the |
directed |
Should the value be directed? |
If calculating slopes associated with OSM data, the results may be better
if the network is first split-up, e.g. using the function
stplanr::rnet_breakup_vertices()
from the
stplanr
package.
Note: The routes
object must have a geometry type of LINESTRING
.
The sf::st_cast()
function can convert from MULTILINESTRING
(and other)
geometries to LINESTRING
s as follows:
r_linestring = sf::st_cast(routes, "LINESTRING")
.
A vector of slopes equal in length to the number simple features (rows representing linestrings) in the input object.
library(sf) routes = lisbon_road_network[1:3, ] dem = dem_lisbon_raster (s = slope_raster(routes, dem)) cor(routes$Avg_Slope, s) slope_raster(routes, dem, directed = TRUE) # Demonstrate that reverse routes have the opposite directed slope slope_raster(st_reverse(routes), dem, directed = TRUE)
library(sf) routes = lisbon_road_network[1:3, ] dem = dem_lisbon_raster (s = slope_raster(routes, dem)) cor(routes$Avg_Slope, s) slope_raster(routes, dem, directed = TRUE) # Demonstrate that reverse routes have the opposite directed slope slope_raster(st_reverse(routes), dem, directed = TRUE)
slope_vector()
calculates the slopes associated with consecutive elements
in one dimensional distance and associated elevations (see examples).
slope_distance()
calculates the slopes associated with consecutive
distances and elevations.
slope_distance_mean()
calculates the mean average slopes associated with
consecutive distances and elevations.
slope_distance_weighted()
calculates the slopes associated with
consecutive distances and elevations,
with the mean value associated with each set of distance/elevation
vectors weighted in proportion to the distance between each elevation
measurement, so longer sections have proportionally more influence
on the resulting gradient estimate (see examples).
slope_vector(x, elevations) slope_distance(d, elevations) slope_distance_mean(d, elevations, directed = FALSE) slope_distance_weighted(d, elevations, directed = FALSE)
slope_vector(x, elevations) slope_distance(d, elevations) slope_distance_mean(d, elevations, directed = FALSE) slope_distance_weighted(d, elevations, directed = FALSE)
x |
Vector of locations |
elevations |
Elevations in same units as x (assumed to be metres) |
d |
Vector of distances between points |
directed |
Should the value be directed? |
A vector of slope gradients associated with each linear element
(each line between consecutive vertices) associated with linear features.
Returned values for slope_distance_mean()
and
slope_distance_mean_weighted()
are summary statistics for all
linear elements in the linestring.
The output value is a proportion representing the change in elevation
for a given change in horizontal movement along the linestring.
0.02, for example, represents a low gradient of 2% while 0.08 represents
a steep gradient of 8%.
x = c(0, 2, 3, 4, 5, 9) elevations = c(1, 2, 2, 4, 3, 0) / 10 # downward slope overall slope_vector(x, elevations) library(sf) m = st_coordinates(lisbon_road_segment) d = sequential_dist(m, lonlat = FALSE) elevations = elevation_extract(m, dem_lisbon_raster) slope_distance(d, elevations) slope_distance_mean(d, elevations) slope_distance_mean(d, elevations, directed = TRUE) slope_distance_mean(rev(d), rev(elevations), directed = TRUE) slope_distance_weighted(d, elevations) slope_distance_weighted(d, elevations, directed = TRUE)
x = c(0, 2, 3, 4, 5, 9) elevations = c(1, 2, 2, 4, 3, 0) / 10 # downward slope overall slope_vector(x, elevations) library(sf) m = st_coordinates(lisbon_road_segment) d = sequential_dist(m, lonlat = FALSE) elevations = elevation_extract(m, dem_lisbon_raster) slope_distance(d, elevations) slope_distance_mean(d, elevations) slope_distance_mean(d, elevations, directed = TRUE) slope_distance_mean(rev(d), rev(elevations), directed = TRUE) slope_distance_weighted(d, elevations) slope_distance_weighted(d, elevations, directed = TRUE)
The function takes a sf object with 'XYZ' coordinates and returns a vector of numeric values representing the average slope of each linestring in the sf data frame input.
slope_xyz( route_xyz, fun = slope_matrix_weighted, lonlat = TRUE, directed = FALSE )
slope_xyz( route_xyz, fun = slope_matrix_weighted, lonlat = TRUE, directed = FALSE )
route_xyz |
An |
fun |
The slope function to calculate per route,
|
lonlat |
Are the coordinates in lon/lat order? TRUE by default |
directed |
Should the value be directed? |
The default function to calculate the mean slope is slope_matrix_weighted()
.
You can also use slope_matrix_mean()
from the package or any other
function that takes the same inputs as these functions not in the package.
A vector of slopes equal in length to the number simple features (rows representing linestrings) in the input object.
route_xyz = lisbon_road_segment_3d slope_xyz(route_xyz, lonlat = FALSE) slope_xyz(route_xyz$geom, lonlat = FALSE) slope_xyz(route_xyz, lonlat = FALSE, directed = TRUE) slope_xyz(route_xyz, lonlat = FALSE, fun = slope_matrix_mean)
route_xyz = lisbon_road_segment_3d slope_xyz(route_xyz, lonlat = FALSE) slope_xyz(route_xyz$geom, lonlat = FALSE) slope_xyz(route_xyz, lonlat = FALSE, directed = TRUE) slope_xyz(route_xyz, lonlat = FALSE, fun = slope_matrix_mean)
The slope_z*()
functions calculate summary values for the Z axis
in sfc
objects with XYZ
geometries.
z_value(x) z_start(x) z_end(x) z_mean(x) z_max(x) z_min(x) z_elevation_change_start_end(x) z_direction(x) z_cumulative_difference(x)
z_value(x) z_start(x) z_end(x) z_mean(x) z_max(x) z_min(x) z_elevation_change_start_end(x) z_direction(x) z_cumulative_difference(x)
x |
An |
A vector of values representing elevations associated with simple feature geometries that have elevations (XYZ coordinates).
x = slopes::lisbon_route_3d x z_value(x)[1:5] xy = slopes::lisbon_route try(z_value(xy)) # error message z_start(x) z_end(x) z_direction(x) z_elevation_change_start_end(x) z_direction(x) z_cumulative_difference(x)
x = slopes::lisbon_route_3d x z_value(x)[1:5] xy = slopes::lisbon_route try(z_value(xy)) # error message z_start(x) z_end(x) z_direction(x) z_elevation_change_start_end(x) z_direction(x) z_cumulative_difference(x)