mapproject {mapproj} | R Documentation |
Converts latitude and longitude into projected coordinates.
mapproject(x, y, projection="", parameters=NULL, orientation=NULL)
x,y |
two vectors giving longitude and latitude coordinates
of points on the earth's surface to be projected.
A list containing components named x and y , giving the
coordinates of the points to be projected may also be given.
Missing values (NA s) are allowed.
The coordinate system is degrees of longitude east of Greenwich
(so the USA is bounded by negative longitudes) and degrees
north of the equator.
|
projection |
optional character string that names a map projection to
use. If the string is "" then the previous projection is used,
with parameters modified by the next two arguments.
|
parameters |
optional numeric vector of parameters for use with the
projection argument.
This argument is optional only in the sense that certain
projections do not require additional parameters.
If a projection does require additional parameters, these
must be given in the parameters argument.
|
orientation |
An optional vector c(latitude,longitude,rotation) which describes
where the "North Pole" should be when computing the projection.
Normally this is c(90,0) , which is appropriate for
cylindrical and conic projections. For a planar projection, you should
set it to the desired point of tangency.
The third value is a clockwise rotation (in degrees), which defaults
to the midrange of the longitude coordinates in the map.
This means that two maps plotted with their own default orientation
may not line up. To avoid this, you should not specify a projection
twice but rather default to the previous projection using
projection="" . See the examples.
|
Each standard projection is displayed with the Prime
Meridian (longitude 0) being a straight vertical line, along which North
is up.
The orientation of nonstandard projections is specified by
the three parameters=c(lat,lon,rot)
.
Imagine a transparent gridded sphere around the globe.
First turn the overlay about the North Pole
so that the Prime Meridian (longitude 0)
of the overlay coincides with meridian lon
on the globe.
Then tilt the North Pole of the
overlay along its Prime Meridian to latitude lat
on the globe.
Finally again turn the
overlay about its "North Pole" so
that its Prime Meridian coincides with the previous position
of (the overlay) meridian rot
.
Project the desired map in
the standard form appropriate to the overlay, but presenting
information from the underlying globe.
In the descriptions that follow (adapted from the McIlroy reference), each projection is shown as a function call; if it requires parameters, these are shown as arguments to the function. The descriptions are grouped into families.
Equatorial projections centered on the Prime Meridian (longitude 0). Parallels are straight horizontal lines.
bonne(0)
lat0
lat0
lat0
Azimuthal projections centered on the North Pole. Parallels are concentric circles. Meridians are equally spaced radial lines.
dist
earth radii from center of earthradius = tan(2 * colatitude)
used in xray crystallographyn
radius = log(colatitude/r)
map from viewing
pedestal of radius r
degreesPolar conic projections symmetric about the Prime Meridian. Parallels are segments of concentric circles. Except in the Bonne projection, meridians are equally spaced radial lines orthogonal to the parallels.
lat0
lat0
and lat1
lat0
and lat1
lat0
and lat1
lat0
developed from tangent coneProjections with bilateral symmetry about the Prime Meridian and the equator.
azequalarea
+lon0
and -lon0
, great circles are
straight lines (a stretched gnomonic projection)+lon0
and -lon0
globular
, circular arc parallels resemble mercator
Doubly periodic conformal projections.
Miscellaneous projections.
dist
earth radii from center of
earth, looking along the Date Line angle
degrees off verticallat0
and lat1
on Prime
Meridianlat
maps to convex lune with given angle
at 90E and 90W
Retroazimuthal projections. At every point the angle between vertical
and a straight line to "Mecca", latitude lat0
on the prime meridian,
is the true bearing of Mecca.
Maps based on the spheroid. Of geodetic quality, these projections do not make sense for tilted orientations.
list with components
named x
and y
, containing the projected coordinates.
NA
s project to NA
s.
Points deemed unprojectable (such as north of 80 degrees
latitude in the Mercator projection) are returned as NA
.
Because of the ambiguity of the first two arguments, the other
arguments must be given by name.
Each time mapproject
is called, it leaves on frame 0 the
dataset .Last.projection
, which is a list with components projection
,
parameters
, and orientation
giving the arguments from the
call to mapproject
or as constructed (for orientation
).
Subsequent calls to mapproject
will get missing information
from .Last.projection
.
Since map
uses mapproject
to do its projections, calls to
mapproject
after a call to map
need not supply any arguments
other than the data.
Tom Minka, An overview of map projections. http://www.stat.cmu.edu/~minka/courses/36-315/handout/handout17.pdf
Richard A. Becker, and Allan R. Wilks, "Maps in S", AT&T Bell Laboratories Statistics Research Report, 1991. http://www.research.att.com/areas/stat/doc/93.2.ps
M. D. McIlroy, documentation for from Tenth Edition UNIX Manual, Volume 1, Saunders College Publishing, 1990.
M. D. McIlroy, Source code for maps and map projections. http://www.cs.dartmouth.edu/~doug/source.html
library(maps) # Bonne equal-area projection with state abbreviations map("state",proj='bonne', param=45) data(state) text(mapproject(state.center), state.abb) # this does not work because the default orientations are different: map("state",proj='bonne', param=45) text(mapproject(state.center,proj='bonne',param=45),state.abb) map("state",proj="albers",par=c(30,40)) map("state",par=c(20,50)) # another Albers projection map("world",proj="gnomonic",orient=c(0,-100,0)) # example of orient # see map.grid for more examples