Type: | Package |
Title: | Spherical Trigonometry |
Version: | 1.5-20 |
Date: | 2024-10-02 |
LinkingTo: | Rcpp |
Imports: | Rcpp, sp |
Depends: | R (≥ 3.0.0) |
Suggests: | methods, raster, terra |
Description: | Spherical trigonometry for geographic applications. That is, compute distances and related measures for angular (longitude/latitude) locations. |
BugReports: | https://github.com/rspatial/geosphere/issues/ |
License: | GPL (≥ 3) |
LazyLoad: | yes |
NeedsCompilation: | yes |
Packaged: | 2024-10-03 02:50:13 UTC; rhijm |
Author: | Robert J. Hijmans [cre, aut], Charles Karney [ctb] (GeographicLib), Ed Williams [ctb], Chris Vennes [ctb] |
Maintainer: | Robert J. Hijmans <r.hijmans@gmail.com> |
Repository: | CRAN |
Date/Publication: | 2024-10-04 06:40:06 UTC |
Geosphere
Description
This package implements functions that compute various aspects of distance, direction, area, etc. for geographic (geodetic) coordinates. Some of the functions are based on an ellipsoid (spheroid) model of the world, other functions use a (simpler, but less accuarate) spherical model. Functions using an ellipsoid can be recognized by having arguments to specify the ellipsoid's radius and flattening (a
and f
). By setting the value for f
to zero, the ellipsoid becomes a sphere.
There are also functions to compute intersections of of rhumb lines. There are also functions to compute the distance between points and polylines, and to characterize spherical polygons; for random sampling on a sphere, and to compute daylength. See the vignette vignette('geosphere')
for examples.
Geographic locations must be specified in latitude and longitude in degrees (NOT radians). Degrees are (obviously) in decimal notation. Thus 12 degrees, 30 minutes, 10 seconds = 12 + 30/60 + 10/3600 = 12.50278 degrees. The Southern and Western hemispheres have a negative sign.
The default unit of distance is meter; but this can be adjusted by supplying a different radius r
to functions.
Directions are expressed in degrees (North = 0 and 360, East = 90, South = 180, and West = 270 degrees).
Acknowledgements
David Purdy, Bill Monahan and others for suggestions to improve the package.
Author(s)
Robert Hijmans, using code by C.F.F. Karney and Chris Veness; formulas by Ed Williams; and with contributions from George Wang, Elias Pipping and others. Maintainer: Robert J. Hijmans <r.hijmans@gmail.com>
References
C.F.F. Karney, 2013. Algorithms for geodesics, J. Geodesy 87: 43-55. doi:10.1007/s00190-012-0578-z. Addenda: https://geographiclib.sourceforge.io/geod-addenda.html. Also see https://geographiclib.sourceforge.io/
https://www.edwilliams.org/avform147.htm
https://www.movable-type.co.uk/scripts/latlong.html
https://en.wikipedia.org/wiki/Great_circle_distance
https://mathworld.wolfram.com/SphericalTrigonometry.html
Ordnance Survey for Great Britain grid reference system
Description
Convert coordinates to the grid reference system used by the Ordnance Survey for Great Britain. Or do the inverse operation to get coordinates for a grid code.
Usage
OSGB(xy, precision, geo=FALSE, inverse=FALSE)
Arguments
xy |
x coordinate pairs (vector, matrix, data.frame |
; or grid codes if inverse=TRUE
.
precision |
character. One of "1m", "5m", "10m", "50m", "100m", "500m", "1km", "5km", "10km", "50km", "100km", "500km" |
geo |
If |
inverse |
If |
Value
character
Examples
pnts <- rbind(cbind(93555 , 256188),
cbind(210637, 349798),
cbind(696457, 481704))
g <- OSGB(pnts, "1km", geo=FALSE)
g
OSGB(g, inverse=TRUE)
Along Track Distance
Description
The "along track distance" is the distance from the start point (p1) to the closest point on the path to a third point (p3),
following a great circle path defined by points p1 and p2. See dist2gc
for the "cross track distance"
Usage
alongTrackDistance(p1, p2, p3, r=6378137)
Arguments
p1 |
longitude/latitude of point(s). Can be a vector of two numbers, a matrix of 2 columns (first one is longitude, second is latitude) or a SpatialPoints* object |
p2 |
as above |
p3 |
as above |
r |
radius of the earth; default = 6378137m |
Value
A distance in units of r (default is meters)
Author(s)
Ed Williams and Robert Hijmans
See Also
Examples
alongTrackDistance(c(0,0),c(60,60),c(50,40))
Antipodes
Description
Compute an antipode, or check whether two points are antipodes. Antipodes are places on Earth that are diametrically opposite to one another; and could be connected by a straight line through the centre of the Earth.
Antipodal points are connected by an infinite number of great circles (e.g. the meridians connecting the poles), and can therefore not be used in some great circle based computations.
Usage
antipode(p)
antipodal(p1, p2, tol=1e-9)
Arguments
p |
Longitude/latitude of a single point, in degrees; can be a vector of two numbers, a matrix of 2 columns (first one is longitude, second is latitude) or a SpatialPoints* object |
p1 |
as above |
p2 |
as above |
tol |
tolerance for equality |
Value
antipodal points or a logical value (TRUE
if antipodal)
Author(s)
Robert Hijmans
References
https://en.wikipedia.org/wiki/Antipodes
Examples
antipode(rbind(c(5,52), c(-120,37), c(-60,0), c(0,70)))
antipodal(c(0,0), c(180,0))
Area of a longitude/latitude polygon
Description
Compute the area of a polygon in angular coordinates (longitude/latitude) on an ellipsoid.
Usage
## S4 method for signature 'matrix'
areaPolygon(x, a=6378137, f=1/298.257223563, ...)
## S4 method for signature 'SpatialPolygons'
areaPolygon(x, a=6378137, f=1/298.257223563, ...)
Arguments
x |
longitude/latitude of the points forming a polygon; Must be a matrix or data.frame of 2 columns (first one is longitude, second is latitude) or a SpatialPolygons* object |
a |
major (equatorial) radius of the ellipsoid |
f |
ellipsoid flattening. The default value is for WGS84 |
... |
Additional arguments. None implemented |
Value
area in square meters
Note
Use raster::area for polygons that have a planar (projected) coordinate reference system.
Author(s)
This function calls GeographicLib code by C.F.F. Karney
References
C.F.F. Karney, 2013. Algorithms for geodesics, J. Geodesy 87: 43-55. doi:10.1007/s00190-012-0578-z. Addenda: https://geographiclib.sourceforge.io/geod-addenda.html. Also see https://geographiclib.sourceforge.io/
See Also
Examples
p <- rbind(c(-180,-20), c(-140,55), c(10, 0), c(-140,-60), c(-180,-20))
areaPolygon(p)
# Be careful with very large polygons, as they may not be what they seem!
# For example, if you wanted a polygon to compute the area equal to about 1/4 of the ellipsoid
# this won't work:
b <- matrix(c(-180, 0, 90, 90, 0, 0, -180, 0), ncol=2, byrow=TRUE)
areaPolygon(b)
# Becausee the shortest path between (-180,0) and (0,0) is
# over one of the poles, not along the equator!
# Inserting a point along the equator fixes that
b <- matrix(c(-180, 0, 0, 0, -90,0, -180, 0), ncol=2, byrow=TRUE)
areaPolygon(b)
Direction of travel
Description
Get the initial bearing (direction; azimuth) to go from point p1
to point p2
(in longitude/latitude) following the shortest path on an ellipsoid (geodetic). Note that the bearing of travel changes continuously while going along the path. A route with constant bearing is a rhumb line (see bearingRhumb
).
Usage
bearing(p1, p2, a=6378137, f=1/298.257223563)
Arguments
p1 |
longitude/latitude of point(s). Can be a vector of two numbers, a matrix of 2 columns (first one is longitude, second is latitude) or a SpatialPoints* object |
p2 |
as above. Can also be missing, in which case the bearing is computed going from the first point to the next and continuing along the following points |
a |
major (equatorial) radius of the ellipsoid. The default value is for WGS84 |
f |
ellipsoid flattening. The default value is for WGS84 |
Value
Bearing in degrees
Note
use f=0
to get a bearing on a sphere (great circle)
Author(s)
Robert Hijmans
References
C.F.F. Karney, 2013. Algorithms for geodesics, J. Geodesy 87: 43-55. doi:10.1007/s00190-012-0578-z. Addenda: https://geographiclib.sourceforge.io/geod-addenda.html. Also see https://geographiclib.sourceforge.io/
See Also
Examples
bearing(c(10,10),c(20,20))
Rhumbline direction
Description
Bearing (direction of travel; true course) along a rhumb line (loxodrome) between two points.
Usage
bearingRhumb(p1, p2)
Arguments
p1 |
longitude/latitude of point(s). Can be a vector of two numbers, a matrix of 2 columns (first one is longitude, second is latitude) or a SpatialPoints* object |
p2 |
as above |
Value
A direction (bearing) in degrees
Note
Unlike most great circles, a rhumb line is a line of constant bearing (direction), i.e. tracks of constant true course. The meridians and the equator are both rhumb lines and great circles. Rhumb lines approaching a pole become a tightly wound spiral.
Author(s)
Chris Veness and Robert Hijmans, based on formulae by Ed Williams
References
https://www.edwilliams.org/avform147.htm#Rhumb
https://en.wikipedia.org/wiki/Rhumb_line
See Also
Examples
bearingRhumb(c(10,10),c(20,20))
Centroid of spherical polygons
Description
Compute the centroid of longitude/latitude polygons. Unlike other functions in this package, there is no spherical trigonometry involved in the implementation of this function. Instead, the function projects the polygon to the (conformal) Mercator coordinate reference system, computes the centroid, and then inversely projects it to longitude and latitude. This approach fails for polygons that include one of the poles (and is rather biased for anything close to the poles). The function should work for polygons that cross the -180/180 meridian (date line).
Usage
centroid(x, ...)
Arguments
x |
SpatialPolygons* object, or a 2-column matrix or data.frame reprenting a single polgyon (longitude/latitude) |
... |
Additional arguments. None implemented |
Value
A matrix (longitude/latitude)
Note
For multi-part polygons, the centroid of the largest part is returned.
Author(s)
Robert J. Hijmans
See Also
Examples
pol <- rbind(c(-180,-20), c(-160,5), c(-60, 0), c(-160,-60), c(-180,-20))
centroid(pol)
Daylength
Description
Compute daylength (photoperiod) for a latitude and date.
Usage
daylength(lat, doy)
Arguments
lat |
latitude, in degrees. I.e. between -90.0 and 90.0 |
doy |
integer, day of the year (1..365) for common (non-leap) years; or an object of class Date; or a character that can be coerced into a date, using 'yyyy-mm-dd' format, e.g. '1982-11-23' |
Value
Daylength in hours
Author(s)
Robert J. Hijmans
References
Forsythe, William C., Edward J. Rykiel Jr., Randal S. Stahl, Hsin-i Wu and Robert M. Schoolfield, 1995. A model comparison for daylength as a function of latitude and day of the year. Ecological Modeling 80:87-95.
Examples
daylength(-25, '2010-10-10')
daylength(45, 1:365)
# average monthly daylength
dl <- daylength(45, 1:365)
tapply(dl, rep(1:12, c(31,28,31,30,31,30,31,31,30,31,30,31)), mean)
Destination given bearing (direction) and distance
Description
Given a start point, initial bearing (direction), and distance, this function computes the destination point travelling along a the shortest path on an ellipsoid (the geodesic).
Usage
destPoint(p, b, d, a=6378137, f=1/298.257223563, ...)
Arguments
p |
Longitude and Latitude of point(s), in degrees. Can be a vector of two numbers, a matrix of 2 columns (first one is longitude, second is latitude) or a SpatialPoints* object |
b |
numeric. Bearing (direction) in degrees |
d |
numeric. Distance in meters |
a |
major (equatorial) radius of the ellipsoid. The default value is for WGS84 |
f |
ellipsoid flattening. The default value is for WGS84 |
... |
additional arguments. If an argument 'r' is supplied, this is taken as the radius of the earth (e.g. 6378137 m) and computations are for a sphere (great circle) instead of an ellipsoid (geodetic). This is for backwards compatibility only |
Value
A pair of coordinates (longitude/latitude)
Note
Direction changes continuously when travelling along a geodesic. Therefore, the final direction is not the same as the initial direction. You can compute the final direction with finalBearing
(see examples, below)
Author(s)
This function calls GeographicLib code by C.F.F. Karney
References
C.F.F. Karney, 2013. Algorithms for geodesics, J. Geodesy 87: 43-55. doi:10.1007/s00190-012-0578-z. Addenda: https://geographiclib.sourceforge.io/geod-addenda.html. Also see https://geographiclib.sourceforge.io/
Examples
p <- cbind(5,52)
d <- destPoint(p,30,10000)
d
#final direction, when arriving at endpoint:
finalBearing(d, p)
Destination along a rhumb line
Description
Calculate the destination point when travelling along a 'rhumb line' (loxodrome), given a start point, direction, and distance.
Usage
destPointRhumb(p, b, d, r = 6378137)
Arguments
p |
longitude/latitude of point(s). Can be a vector of two numbers, a matrix of 2 columns (first one is longitude, second is latitude) or a SpatialPoints* object |
b |
bearing (direction) in degrees |
d |
distance; in the same unit as |
r |
radius of the earth; default = 6378137 m |
Value
Coordinates (longitude/latitude) of a point
Author(s)
Chris Veness; ported to R by Robert Hijmans
References
https://www.edwilliams.org/avform147.htm#Rhumb
https://www.movable-type.co.uk/scripts/latlong.html
https://en.wikipedia.org/wiki/Rhumb_line
See Also
Examples
destPointRhumb(c(0,0), 30, 100000, r = 6378137)
Distance between points and lines or the border of polygons.
Description
The shortest distance between points and polylines or polygons.
Usage
dist2Line(p, line, distfun=distGeo)
Arguments
p |
longitude/latitude of point(s). Can be a vector of two numbers, a matrix of 2 columns (first one is longitude, second is latitude) or a SpatialPoints* object |
line |
longitude/latitude of line as a matrix of 2 columns (first one is longitude, second is latitude) or a SpatialLines* or SpatialPolygons* object |
distfun |
A distance function, such as distGeo |
Value
matrix with distance and lon/lat of the nearest point on the line. Distance is in the same unit as r
in the distfun
(default is meters). If line
is a Spatial*
object, the ID (index) of (one of) the nearest objects is also returned. Thus if the objects are polygons and the point is inside a polygon the function may return the ID of a neighboring polygon that shares the nearest border. You can use the intersect
function in packages terra
.
Author(s)
George Wang and Robert Hijmans
See Also
Examples
line <- rbind(c(-180,-20), c(-150,-10), c(-140,55), c(10, 0), c(-140,-60))
pnts <- rbind(c(-170,0), c(-75,0), c(-70,-10), c(-80,20), c(-100,-50),
c(-100,-60), c(-100,-40), c(-100,-20), c(-100,-10), c(-100,0))
d = dist2Line(pnts, line)
plot( makeLine(line), type='l')
points(line)
points(pnts, col='blue', pch=20)
points(d[,2], d[,3], col='red', pch='x')
for (i in 1:nrow(d)) lines(gcIntermediate(pnts[i,], d[i,2:3], 10), lwd=2)
Cross Track Distance
Description
Compute the distance of a point to a great-circle path (also referred to as the cross track distance or cross track error). The great circle is defined by p1
and p2
, while p3
is the point away from the path.
Usage
dist2gc(p1, p2, p3, r=6378137, sign=FALSE)
Arguments
p1 |
Start of great circle path. longitude/latitude of point(s). Can be a vector of two numbers, a matrix of 2 columns (first one is longitude, second is latitude) or a SpatialPoints* object |
p2 |
End of great circle path. As above |
p3 |
Point away from the great cricle path. As for p2 |
r |
radius of the earth; default = 6378137 |
sign |
logical. If |
Value
A distance in units of r
(default is meters)
If sign=TRUE
, the sign indicates which side of the path p3 is on. Positive means right of the course from p1 to p2, negative means left.
Author(s)
Ed Williams and Robert Hijmans
References
https://www.movable-type.co.uk/scripts/latlong.html
https://www.edwilliams.org/ftp/avsig/avform.txt
See Also
Examples
dist2gc(c(0,0),c(90,90),c(80,80))
'Law of cosines' great circle distance
Description
The shortest distance between two points (i.e., the 'great-circle-distance' or 'as the crow flies'), according to the 'law of the cosines'. This method assumes a spherical earth, ignoring ellipsoidal effects.
Usage
distCosine(p1, p2, r=6378137)
Arguments
p1 |
longitude/latitude of point(s). Can be a vector of two numbers, a matrix of 2 columns (first one is longitude, second is latitude) or a SpatialPoints* object |
p2 |
as above |
r |
radius of the earth; default = 6378137 m |
Value
Vector of distances in the same unit as r
(default is meters)
Author(s)
Robert Hijmans
References
https://en.wikipedia.org/wiki/Great_circle_distance
See Also
distGeo, distHaversine, distVincentySphere, distVincentyEllipsoid, distMeeus
Examples
distCosine(c(0,0),c(90,90))
Distance on an ellipsoid (the geodesic)
Description
Highly accurate estimate of the shortest distance between two points on an ellipsoid (default is WGS84 ellipsoid). The shortest path between two points on an ellipsoid is called the geodesic.
Usage
distGeo(p1, p2, a=6378137, f=1/298.257223563)
Arguments
p1 |
longitude/latitude of point(s). Can be a vector of two numbers, a matrix of 2 columns (first column is longitude, second column is latitude) or a SpatialPoints* object |
p2 |
as above; or missing, in which case the sequential distance between the points in p1 is computed |
a |
numeric. Major (equatorial) radius of the ellipsoid. The default value is for WGS84 |
f |
numeric. Ellipsoid flattening. The default value is for WGS84 |
Details
Parameters from the WGS84 ellipsoid are used by default. It is the best available global ellipsoid, but for some areas other ellipsoids could be preferable, or even necessary if you work with a printed map that refers to that ellipsoid. Here are parameters for some commonly used ellipsoids. Also see the refEllipsoids
function.
ellipsoid | a | f |
|
WGS84 | 6378137 | 1/298.257223563 |
|
GRS80 | 6378137 | 1/298.257222101 |
|
GRS67 | 6378160 | 1/298.25 |
|
Airy 1830 | 6377563.396 | 1/299.3249646 |
|
Bessel 1841 | 6377397.155 | 1/299.1528434 |
|
Clarke 1880 | 6378249.145 | 1/293.465 |
|
Clarke 1866 | 6378206.4 | 1/294.9786982 |
|
International 1924 | 6378388 | 1/297 |
|
Krasovsky 1940 | 6378245 | 1/298.2997381 |
|
more info: https://en.wikipedia.org/wiki/Reference_ellipsoid
Value
Vector of distances in meters
Author(s)
This function calls GeographicLib code by C.F.F. Karney
References
C.F.F. Karney, 2013. Algorithms for geodesics, J. Geodesy 87: 43-55. doi:10.1007/s00190-012-0578-z. Addenda: https://geographiclib.sourceforge.io/geod-addenda.html. Also see https://geographiclib.sourceforge.io/
See Also
distCosine, distHaversine, distVincentySphere, distVincentyEllipsoid, distMeeus
Examples
distGeo(c(0,0),c(90,90))
'Haversine' great circle distance
Description
The shortest distance between two points (i.e., the 'great-circle-distance' or 'as the crow flies'), according to the 'haversine method'. This method assumes a spherical earth, ignoring ellipsoidal effects.
Usage
distHaversine(p1, p2, r=6378137)
Arguments
p1 |
longitude/latitude of point(s). Can be a vector of two numbers, a matrix of 2 columns (first one is longitude, second is latitude) or a SpatialPoints* object |
p2 |
as above; or missing, in which case the sequential distance between the points in p1 is computed |
r |
radius of the earth; default = 6378137 m |
Details
The Haversine ('half-versed-sine') formula was published by R.W. Sinnott in 1984, although it has been known for much longer. At that time computational precision was lower than today (15 digits precision). With current precision, the spherical law of cosines formula appears to give equally good results down to very small distances. If you want greater accuracy, you could use the distVincentyEllipsoid
method.
Value
Vector of distances in the same unit as r
(default is meters)
Author(s)
Chris Veness and Robert Hijmans
References
Sinnott, R.W, 1984. Virtues of the Haversine. Sky and Telescope 68(2): 159
https://www.movable-type.co.uk/scripts/latlong.html
https://en.wikipedia.org/wiki/Great_circle_distance
See Also
distGeo, distCosine, distVincentySphere, distVincentyEllipsoid, distMeeus
Examples
distHaversine(c(0,0),c(90,90))
'Meeus' great circle distance
Description
The shortest distance between two points on an ellipsoid (the 'geodetic'), according to the 'Meeus' method. distGeo
should be more accurate.
Usage
distMeeus(p1, p2, a=6378137, f=1/298.257223563)
Arguments
p1 |
longitude/latitude of point(s), in degrees 1; can be a vector of two numbers, a matrix of 2 columns (first one is longitude, second is latitude) or a SpatialPoints* object |
p2 |
as above; or missing, in which case the sequential distance between the points in p1 is computed |
a |
numeric. Major (equatorial) radius of the ellipsoid. The default value is for WGS84 |
f |
numeric. Ellipsoid flattening. The default value is for WGS84 |
Details
Parameters from the WGS84 ellipsoid are used by default. It is the best available global ellipsoid, but for some areas other ellipsoids could be preferable, or even necessary if you work with a printed map that refers to that ellipsoid. Here are parameters for some commonly used ellipsoids:
ellipsoid | a | f |
|
WGS84 | 6378137 | 1/298.257223563 |
|
GRS80 | 6378137 | 1/298.257222101 |
|
GRS67 | 6378160 | 1/298.25 |
|
Airy 1830 | 6377563.396 | 1/299.3249646 |
|
Bessel 1841 | 6377397.155 | 1/299.1528434 |
|
Clarke 1880 | 6378249.145 | 1/293.465 |
|
Clarke 1866 | 6378206.4 | 1/294.9786982 |
|
International 1924 | 6378388 | 1/297 |
|
Krasovsky 1940 | 6378245 | 1/298.2997381 |
|
more info: https://en.wikipedia.org/wiki/Reference_ellipsoid
Value
Distance value in the same units as parameter a
of the ellipsoid (default is meters)
Note
This algorithm is also used in the spDists
function in the sp package
Author(s)
Robert Hijmans, based on a script by Stephen R. Schmitt
References
Meeus, J., 1999 (2nd edition). Astronomical algoritms. Willman-Bell, 477p.
See Also
distGeo, distVincentyEllipsoid, distVincentySphere, distHaversine, distCosine
Examples
distMeeus(c(0,0),c(90,90))
# on a 'Clarke 1880' ellipsoid
distMeeus(c(0,0),c(90,90), a=6378249.145, f=1/293.465)
Distance along a rhumb line
Description
A rhumb line (loxodrome) is a path of constant bearing (direction), which crosses all meridians at the same angle.
Usage
distRhumb(p1, p2, r=6378137)
Arguments
p1 |
longitude/latitude of point(s). Can be a vector of two numbers, a matrix of 2 columns (first one is longitude, second is latitude) or a SpatialPoints* object |
p2 |
as above; or missing, in which case the sequential distance between the points in p1 is computed |
r |
radius of the earth; default = 6378137 m |
Details
Rhumb (from the Spanish word for course, 'rumbo') lines are straight lines on a Mercator projection map. They were used in navigation because it is easier to follow a constant compass bearing than to continually adjust the bearing as is needed to follow a great circle, even though rhumb lines are normally longer than great-circle (orthodrome) routes. Most rhumb lines will gradually spiral towards one of the poles.
Value
distance in units of r (default=meters)
Author(s)
Robert Hijmans and Chris Veness
References
https://www.movable-type.co.uk/scripts/latlong.html
See Also
distCosine, distHaversine, distVincentySphere, distVincentyEllipsoid
Examples
distRhumb(c(10,10),c(20,20))
'Vincenty' (ellipsoid) great circle distance
Description
The shortest distance between two points (i.e., the 'great-circle-distance' or 'as the crow flies'), according to the 'Vincenty (ellipsoid)' method. This method uses an ellipsoid and the results are very accurate. The method is computationally more intensive than the other great-circled methods in this package.
Usage
distVincentyEllipsoid(p1, p2, a=6378137, b=6356752.3142, f=1/298.257223563)
Arguments
p1 |
longitude/latitude of point(s), in degrees 1; can be a vector of two numbers, a matrix of 2 columns (first one is longitude, second is latitude) or a SpatialPoints* object |
p2 |
as above; or missing, in which case the sequential distance between the points in p1 is computed |
a |
Equatorial axis of ellipsoid |
b |
Polar axis of ellipsoid |
f |
Inverse flattening of ellipsoid |
Details
The WGS84 ellipsoid is used by default. It is the best available global ellipsoid, but for some areas other ellipsoids could be preferable, or even necessary if you work with a printed map that refers to that ellipsoid. Here are parameters for some commonly used ellipsoids:
ellipsoid | a | b | f |
|
WGS84 | 6378137 | 6356752.3142 | 1/298.257223563 |
|
GRS80 | 6378137 | 6356752.3141 | 1/298.257222101 |
|
GRS67 | 6378160 | 6356774.719 | 1/298.25 |
|
Airy 1830 | 6377563.396 | 6356256.909 | 1/299.3249646 |
|
Bessel 1841 | 6377397.155 | 6356078.965 | 1/299.1528434 |
|
Clarke 1880 | 6378249.145 | 6356514.86955 | 1/293.465 |
|
Clarke 1866 | 6378206.4 | 6356583.8 | 1/294.9786982 |
|
International 1924 | 6378388 | 6356911.946 | 1/297 |
|
Krasovsky 1940 | 6378245 | 6356863 | 1/298.2997381 |
|
a
is the 'semi-major axis', and b
is the 'semi-minor axis' of the ellipsoid. f
is the flattening.
Note that f = (a-b)/a
more info: https://en.wikipedia.org/wiki/Reference_ellipsoid
Value
Distance value in the same units as the ellipsoid (default is meters)
Author(s)
Chris Veness and Robert Hijmans
References
Vincenty, T. 1975. Direct and inverse solutions of geodesics on the ellipsoid with application of nested equations. Survey Review Vol. 23, No. 176, pp88-93. Available here:
https://www.movable-type.co.uk/scripts/latlong-vincenty.html
https://en.wikipedia.org/wiki/Great_circle_distance
See Also
distGeo, distVincentySphere, distHaversine, distCosine, distMeeus
Examples
distVincentyEllipsoid(c(0,0),c(90,90))
# on a 'Clarke 1880' ellipsoid
distVincentyEllipsoid(c(0,0),c(90,90), a=6378249.145, b=6356514.86955, f=1/293.465)
'Vincenty' (sphere) great circle distance
Description
The shortest distance between two points (i.e., the 'great-circle-distance' or 'as the crow flies'), according to the 'Vincenty (sphere)' method.
This method assumes a spherical earth, ignoring ellipsoidal effects and it is less accurate then the distVicentyEllipsoid
method.
Usage
distVincentySphere(p1, p2, r=6378137)
Arguments
p1 |
longitude/latitude of point(s). Can be a vector of two numbers, a matrix of 2 columns (first one is longitude, second is latitude) or a SpatialPoints* object |
p2 |
as above; or missing, in which case the sequential distance between the points in p1 is computed |
r |
radius of the earth; default = 6378137 m |
Value
Distance value in the same unit as r
(default is meters)
Author(s)
Robert Hijmans
References
https://en.wikipedia.org/wiki/Great_circle_distance
See Also
distGeo, distVincentyEllipsoid, distHaversine, distCosine, distMeeus
Examples
distVincentySphere(c(0,0),c(90,90))
Distance matrix
Description
Distance matrix of a set of points, or between two sets of points
Usage
distm(x, y, fun=distGeo)
Arguments
x |
longitude/latitude of point(s). Can be a vector of two numbers, a matrix of 2 columns (first one is longitude, second is latitude) or a SpatialPoints* object |
y |
Same as |
fun |
A function to compute distances (e.g., distCosine or distGeo) |
Value
Matrix of distances
Author(s)
Robert Hijmans
References
https://en.wikipedia.org/wiki/Great_circle_distance
See Also
distGeo, distCosine, distHaversine, distVincentySphere, distVincentyEllipsoid
Examples
xy <- rbind(c(0,0),c(90,90),c(10,10),c(-120,-45))
distm(xy)
xy2 <- rbind(c(0,0),c(10,-10))
distm(xy, xy2)
Final direction
Description
Get the final direction (bearing) when arriving at p2
after starting from p1
and following the shortest path on an ellipsoid (following a geodetic) or on a sphere (following a great circle).
Usage
finalBearing(p1, p2, a=6378137, f=1/298.257223563, sphere=FALSE)
Arguments
p1 |
longitude/latitude of point(s). Can be a vector of two numbers, a matrix of 2 columns (first column is longitude, second column is latitude) or a SpatialPoints* object |
p2 |
as above |
a |
major (equatorial) radius of the ellipsoid. The default value is for WGS84 |
f |
ellipsoid flattening. The default value is for WGS84 |
sphere |
logical. If |
Value
A vector of directions (bearings) in degrees
Author(s)
This function calls GeographicLib code by C.F.F. Karney
References
C.F.F. Karney, 2013. Algorithms for geodesics, J. Geodesy 87: 43-55. doi:10.1007/s00190-012-0578-z. Addenda: https://geographiclib.sourceforge.io/geod-addenda.html. Also see https://geographiclib.sourceforge.io/
See Also
Examples
bearing(c(10,10),c(20,20))
finalBearing(c(10,10),c(20,20))
Intersections of two great circles
Description
Get the two points where two great cricles cross each other. Great circles are defined by two points on it.
Usage
gcIntersect(p1, p2, p3, p4)
Arguments
p1 |
Longitude/latitude of a single point, in degrees; can be a vector of two numbers, a matrix of 2 columns (first one is longitude, second is latitude) or a SpatialPoints* object |
p2 |
As above |
p3 |
As above |
p4 |
As above |
Value
two points for each pair of great circles
Author(s)
Robert Hijmans, based on equations by Ed Williams (see reference)
References
https://www.edwilliams.org/intersect.htm
See Also
Examples
p1 <- c(5,52); p2 <- c(-120,37); p3 <- c(-60,0); p4 <- c(0,70)
gcIntersect(p1,p2,p3,p4)
Intersections of two great circles
Description
Get the two points where two great cricles cross each other. In this function, great circles are defined by a points and an initial bearing. In function gcIntersect
they are defined by two sets of points.
Usage
gcIntersectBearing(p1, brng1, p2, brng2)
Arguments
p1 |
longitude/latitude of point(s). Can be a vector of two numbers, a matrix of 2 columns (first one is longitude, second is latitude) or a SpatialPoints* object |
brng1 |
Bearing from p1 |
p2 |
As above. Should have same length as p1, or a single point (or vice versa when p1 is a single point |
brng2 |
Bearing from p2 |
Value
a matrix with four columns (two points)
Author(s)
Chris Veness and Robert Hijmans based on code by Ed Williams
References
https://www.edwilliams.org/avform147.htm#Intersection
https://www.movable-type.co.uk/scripts/latlong.html
See Also
Examples
gcIntersectBearing(c(10,0), 10, c(-10,0), 10)
Latitude on a Great Circle
Description
Latitude at which a great circle crosses a longitude
Usage
gcLat(p1, p2, lon)
Arguments
p1 |
Longitude/latitude of a single point, in degrees; can be a vector of two numbers, a matrix of 2 columns (first one is longitude, second is latitude) or a SpatialPoints* object |
p2 |
As above |
lon |
Longitude |
Value
A numeric (latitude)
Author(s)
Robert Hijmans based on a formula by Ed Williams
References
https://www.edwilliams.org/avform147.htm#Int
See Also
Examples
gcLat(c(5,52), c(-120,37), lon=-120)
Longitude on a Great Circle
Description
Longitudes at which a great circle crosses a latitude (parallel)
Usage
gcLon(p1, p2, lat)
Arguments
p1 |
longitude/latitude of point(s). Can be a vector of two numbers, a matrix of 2 columns (first one is longitude, second is latitude) or a SpatialPoints* object |
p2 |
as above |
lat |
a latitude |
Value
vector of two numbers (longitudes)
Author(s)
Robert Hijmans based on code by Ed Williams
References
https://www.edwilliams.org/avform147.htm#Intersection
See Also
Examples
gcLon(c(5,52), c(-120,37), 40)
Highest latitude on a great circle
Description
What is northern most point that will be reached when following a great circle? Computed with Clairaut's formula. The southern most point is the antipode
of the northern-most point. This does not seem to be very precise; and you could use optimization instead to find this point (see examples)
Usage
gcMaxLat(p1, p2)
Arguments
p1 |
longitude/latitude of point(s). Can be a vector of two numbers, a matrix of 2 columns (first one is longitude, second is latitude) or a SpatialPoints* object |
p2 |
as above |
Value
A matrix with coordinates (longitude/latitude)
Author(s)
Ed Williams, Chris Veness, Robert Hijmans
References
https://www.edwilliams.org/ftp/avsig/avform.txt
https://www.movable-type.co.uk/scripts/latlong.html
See Also
Examples
gcMaxLat(c(5,52), c(-120,37))
# Another way to get there:
f <- function(lon){gcLat(c(5,52), c(-120,37), lon)}
optimize(f, interval=c(-180, 180), maximum=TRUE)
geodesic and inverse geodesic problem
Description
Highly accurate estimate of the 'geodesic problem' (find location and azimuth at arrival when departing from a location, given an direction (azimuth) at departure and distance) and the 'inverse geodesic problem' (find the distance between two points and the azimuth of departure and arrival for the shortest path. Computations are for an ellipsoid (default is WGS84 ellipsoid).
This is a direct implementation of the the GeographicLib code by C.F.F. Karney that is also used in several other functions in this package (for example, in distGeo
and areaPolygon
).
Usage
geodesic(p, azi, d, a=6378137, f=1/298.257223563, ...)
geodesic_inverse(p1, p2, a=6378137, f=1/298.257223563, ...)
Arguments
p |
longitude/latitude of point(s). Can be a vector of two numbers, a matrix of 2 columns (first column is longitude, second column is latitude) or a SpatialPoints* object |
p1 |
as above |
p2 |
as above |
azi |
numeric. Azimuth of departure in degrees |
d |
numeric. Distance in meters |
a |
numeric. Major (equatorial) radius of the ellipsoid. The default value is for WGS84 |
f |
numeric. Ellipsoid flattening. The default value is for WGS84 |
... |
additional arguments (none implemented) |
Details
Parameters from the WGS84 ellipsoid are used by default. It is the best available global ellipsoid, but for some areas other ellipsoids could be preferable, or even necessary if you work with a printed map that refers to that ellipsoid. Here are parameters for some commonly used ellipsoids.
ellipsoid | a | f |
|
WGS84 | 6378137 | 1/298.257223563 |
|
GRS80 | 6378137 | 1/298.257222101 |
|
GRS67 | 6378160 | 1/298.25 |
|
Airy 1830 | 6377563.396 | 1/299.3249646 |
|
Bessel 1841 | 6377397.155 | 1/299.1528434 |
|
Clarke 1880 | 6378249.145 | 1/293.465 |
|
Clarke 1866 | 6378206.4 | 1/294.9786982 |
|
International 1924 | 6378388 | 1/297 |
|
Krasovsky 1940 | 6378245 | 1/298.2997381 |
|
more info: https://en.wikipedia.org/wiki/Reference_ellipsoid
Value
Three column matrix with columns 'longitude', 'latitude', 'azimuth' (geodesic); or 'distance' (in meters), 'azimuth1' (of departure), 'azimuth2' (of arrival) (geodesic_inverse)
Author(s)
This function calls GeographicLib code by C.F.F. Karney
References
C.F.F. Karney, 2013. Algorithms for geodesics, J. Geodesy 87: 43-55. doi:10.1007/s00190-012-0578-z. Addenda: https://geographiclib.sourceforge.io/geod-addenda.html. Also see https://geographiclib.sourceforge.io/
See Also
Examples
geodesic(cbind(0,0), 30, 1000000)
geodesic_inverse(cbind(0,0), cbind(90,90))
Mean location of sperhical coordinates
Description
mean location for spherical (longitude/latitude) coordinates that deals with the angularity. I.e., the mean of longitudes -179 and 178 is 179.5
Usage
geomean(xy, w)
Arguments
xy |
matrix with two columns (longitude/latitude), or a SpatialPoints or SpatialPolygons object with a longitude/latitude CRS |
w |
weights (vector of numeric values, with a length that is equal to the number of spatial features in |
Value
Ccoordinate pair (numeric)
Author(s)
Robert J. Hijmans
Examples
xy <- cbind(x=c(-179,179, 177), y=c(12,14,16))
xy
geomean(xy)
Great circle
Description
Get points on a great circle as defined by the shortest distance between two specified points
Usage
greatCircle(p1, p2, n=360, sp=FALSE)
Arguments
p1 |
longitude/latitude of point(s). Can be a vector of two numbers, a matrix of 2 columns (first one is longitude, second is latitude) or a SpatialPoints* object |
p2 |
as above |
n |
The requested number of points on the Great Circle |
sp |
Logical. Return a SpatialLines object? |
Value
A matrix of points, or a list of such matrices (e.g., if multiple bearings are supplied)
Author(s)
Robert Hijmans, based on a formula provided by Ed Williams
References
https://www.edwilliams.org/avform147.htm#Int
Examples
greatCircle(c(5,52), c(-120,37), n=36)
Great circle
Description
Get points on a great circle as defined by a point and an initial bearing
Usage
greatCircleBearing(p, brng, n=360)
Arguments
p |
longitude/latitude of a single point. Can be a vector of two numbers, a matrix of 2 columns (first one is longitude, second is latitude) or a SpatialPoints* object |
brng |
bearing |
n |
The requested number of points on the great circle |
Value
A matrix of points, or a list of matrices (e.g., if multiple bearings are supplied)
Author(s)
Robert Hijmans based on formulae by Ed Williams
References
https://www.edwilliams.org/avform147.htm#Int
Examples
greatCircleBearing(c(5,52), 45, n=12)
Distance to the horizon
Description
Empirical function to compute the distance to the horizon from a given altitude. The earth is assumed to be smooth, i.e. mountains and other obstacles are ignored.
Usage
horizon(h, r=6378137)
Arguments
h |
altitude, numeric >= 0. Should have the same unit as r |
r |
radius of the earth; default value is 6378137 m |
Value
Distance in units of h
(default is meters)
Author(s)
Robert J. Hijmans
References
https://www.edwilliams.org/avform147.htm#Horizon
Bowditch, 1995. American Practical Navigator. Table 12.
Examples
horizon(1.80) # me
horizon(324) # Eiffel tower
Intermediate points on a great circle (sphere)
Description
Get intermediate points (way points) between the two locations with longitude/latitude coordinates. gcIntermediate is based on a spherical model of the earth and internally uses distCosine
.
Usage
gcIntermediate(p1, p2, n=50, breakAtDateLine=FALSE, addStartEnd=FALSE, sp=FALSE, sepNA)
Arguments
p1 |
longitude/latitude of a single point, in degrees. This can be a vector of two numbers, a matrix of 2 columns (first one is longitude, second is latitude) or a SpatialPoints* object |
p2 |
as for |
n |
integer. The desired number of intermediate points |
breakAtDateLine |
logical. Return two matrices if the dateline is crossed? |
addStartEnd |
logical. Add p1 and p2 to the result? |
sp |
logical. Return a SpatialLines object? |
sepNA |
logical. Rather than as a list, return the values as a two column matrix with lines seperated by a row of NA values? (for use in 'plot') |
Value
matrix or list with intermediate points
Author(s)
Robert Hijmans based on code by Ed Williams (great circle)
References
https://www.edwilliams.org/avform147.htm#Intermediate
Examples
gcIntermediate(c(5,52), c(-120,37), n=6, addStartEnd=TRUE)
Length of lines
Description
Compute the length of lines
Usage
lengthLine(line)
Arguments
line |
longitude/latitude of line as a matrix of 2 columns (first one is longitude, second is latitude) or a SpatialLines* or SpatialPolygons* object |
Value
length (in meters) for each line
See Also
For planar coordinates, see the terra or sf packages
Examples
line <- rbind(c(-180,-20), c(-150,-10), c(-140,55), c(10, 0), c(-140,-60))
d <- lengthLine(line)
Add vertices to a polygon or line
Description
Make a polygon or line by adding intermedate points (vertices) on the great circles inbetween the points supplied. This can be relevant when vertices are relatively far apart.
It can make the shape of the object to be accurate, when plotted on a plane. makePoly
will also close the polygon if needed.
Usage
makePoly(p, interval=10000, sp=FALSE, ...)
makeLine(p, interval=10000, sp=FALSE, ...)
Arguments
p |
a 2-column matrix (longitude/latitude) or a SpatialPolygons or SpatialLines object |
interval |
maximum interval of points, in units of r |
sp |
Logical. If |
... |
additional arguments passed to distGeo |
Value
A matrix
Author(s)
Robert J. Hijmans
Examples
pol <- rbind(c(-180,-20), c(-160,5), c(-60, 0), c(-160,-60), c(-180,-20))
plot(pol)
lines(pol, col='red', lwd=3)
pol2 = makePoly(pol, interval=100000)
lines(pol2, col='blue', lwd=2)
Mercator projection
Description
Transform longitude/latiude points to the Mercator projection. The main purpose of this function is to compute centroids, and to illustrate rhumb lines in the vignette.
Usage
mercator(p, inverse=FALSE, r=6378137)
Arguments
p |
longitude/latitude of point(s). Can be a vector of two numbers, a matrix of 2 columns (first one is longitude, second is latitude) or a SpatialPoints* object |
inverse |
Logical. If |
r |
Numeric. Radius of the earth; default = 6378137 m |
Value
matrix
Author(s)
Robert Hijmans
Examples
a = mercator(c(5,52))
a
mercator(a, inverse=TRUE)
Mid-point
Description
Find the point half-way between two points along an ellipsoid
Usage
midPoint(p1, p2, a=6378137, f = 1/298.257223563)
Arguments
p1 |
longitude/latitude of point(s). Can be a vector of two numbers, a matrix of 2 columns (first one is longitude, second is latitude) or a SpatialPoints* object |
p2 |
As above |
a |
major (equatorial) radius of the ellipsoid |
f |
ellipsoid flattening. The default value is for WGS84 |
Value
matrix with coordinate pairs
Author(s)
Elias Pipping and Robert Hijmans
Examples
midPoint(c(0,0),c(90,90))
midPoint(c(0,0),c(90,90), f=0)
Is a point on a given great circle?
Description
Test if a point is on a great circle defined by two other points.
Usage
onGreatCircle(p1, p2, p3, tol=0.0001)
Arguments
p1 |
Longitude/latitude of the first point defining a great circle, in degrees; can be a vector of two numbers, a matrix of 2 columns (first one is longitude, second is latitude) or a SpatialPoints* object |
p2 |
as above for the second point |
p3 |
the point(s) to be tested if they are on the great circle or not |
tol |
numeric. maximum distance from the great circle (in degrees) that is tolerated to be considered on the circle |
Value
logical
Author(s)
Robert Hijmans
Examples
onGreatCircle(c(0,0), c(30,30), rbind(c(-10 -11.33812), c(10,20)))
Compute the perimeter of a longitude/latitude polygon
Description
Compute the perimeter of a polygon (or the length of a line) with longitude/latitude coordinates, on an ellipsoid (WGS84 by default)
Usage
## S4 method for signature 'matrix'
perimeter(x, a=6378137, f=1/298.257223563, ...)
## S4 method for signature 'SpatialPolygons'
perimeter(x, a=6378137, f=1/298.257223563, ...)
## S4 method for signature 'SpatialLines'
perimeter(x, a=6378137, f=1/298.257223563, ...)
Arguments
x |
Longitude/latitude of the points forming a polygon or line; Must be a matrix of 2 columns (first one is longitude, second is latitude) or a SpatialPolygons* or SpatialLines* object |
a |
major (equatorial) radius of the ellipsoid. The default value is for WGS84 |
f |
ellipsoid flattening. The default value is for WGS84 |
... |
Additional arguments. None implemented |
Value
Numeric. The perimeter or length in m.
Author(s)
This function calls GeographicLib code by C.F.F. Karney
References
C.F.F. Karney, 2013. Algorithms for geodesics, J. Geodesy 87: 43-55. doi:10.1007/s00190-012-0578-z. Addenda: https://geographiclib.sourceforge.io/geod-addenda.html. Also see https://geographiclib.sourceforge.io/
See Also
Examples
xy <- rbind(c(-180,-20), c(-140,55), c(10, 0), c(-140,-60), c(-180,-20))
perimeter(xy)
Plot
Description
Plot polygons with arrow heads on each line segment, pointing towards the next vertex. This shows the direction of each line segment.
Usage
plotArrows(p, fraction=0.9, length=0.15, first='', add=FALSE, ...)
Arguments
p |
Polygons (either a 2 column matrix or data.frame; or a SpatialPolygons* object |
fraction |
numeric between 0 and 1. When smaller then 1, interrupted lines are drawn |
length |
length of the edges of the arrow head (in inches) |
first |
Character to plot on first (and last) vertex |
add |
Logical. If |
... |
Additional arguments, see Details |
Note
Based on an example in Software for Data Analysis by John Chambers (pp 250-251) but adjusted such that the line segments follow great circles between vertices.
Author(s)
Robert J. Hijmans
Examples
pol <- rbind(c(-180,-20), c(-160,5), c(-60, 0), c(-160,-60), c(-180,-20))
plotArrows(pol)
Random or regularly distributed coordinates on the globe
Description
randomCoordinates returns a 'uniform random sample' in the sense that the probability that a point is drawn from any region is equal to the area of that region divided by the area of the entire sphere. This would not happen if you took a random uniform sample of longitude and latitude, as the sample would be biased towards the poles.
regularCoordiaates returns a set of coordinates that are regularly distributed on the globe.
Usage
randomCoordinates(n)
regularCoordinates(N)
Arguments
n |
Sample size (number of points (coordinate pairs)) |
N |
Number of 'parts' in which the earth is subdived ) |
Value
Matrix of lon/lat coordiantes
Author(s)
Robert Hijmans, based on code by Nils Haeck (regularCoordinates) and on suggstions by Michael Orion (randomCoordinates)
Examples
randomCoordinates(3)
regularCoordinates(1)
Reference ellipsoids
Description
This function returns a data.frame with parameters a
(semi-major axis) and 1/f
(inverse flattening) for a set of reference ellipsoids.
Usage
refEllipsoids()
Value
data.frame
Note
To compute parameter b
you can do
Author(s)
Robert J. Hijmans
See Also
Examples
e <- refEllipsoids()
e[e$code=='WE', ]
#to compute semi-minor axis b:
e$b <- e$a - e$a / e$invf
Span of polygons
Description
Compute the approximate surface span of polygons in longitude and latitude direction. Span is computed by rasterizing the polygons; and precision increases with the number of 'scan lines'. You can either use a fixed number of scan lines for each polygon, or a fixed band-width.
Usage
span(x, ...)
Arguments
x |
a SpatialPolygons* object or a 2-column matrix (longitude/latitude) |
... |
Additional arguments, see Details |
Details
The following additional arguments can be passed, to replace default values for this function
nbands | Character. Method to determine the number of bands to 'scan' the polygon. Either 'fixed' or 'variable' | |
n | Integer >= 1. If nbands='fixed' , how many bands should be used |
|
res | Numeric. If nbands='variable' , what should the bandwidth be (in degrees)? |
|
fun | Logical. A function such as mean or min. Mean computes the average span | |
... | further additional arguments passed to distGeo | |
Value
A list, or a matrix if a function fun
is specified. Values are in the units of r
(default is meter)
Author(s)
Robert J. Hijmans
Examples
pol <- rbind(c(-180,-20), c(-160,5), c(-60, 0), c(-160,-60), c(-180,-20))
plot(pol)
lines(pol)
# lon and lat span in m
span(pol, fun=max)
x <- span(pol)
max(x$latspan)
mean(x$latspan)
plot(x$longitude, x$lonspan)
World countries
Description
world coastline and country outlines in longitude/latitude (wrld) and in Mercator projection (merc).
Usage
data(wrld)
data(merc)
Source
Derived from the wrld_simpl data set in package maptools