cmdscale {stats}  R Documentation 
Classical multidimensional scaling (MDS) of a data matrix. Also known as principal coordinates analysis (Gower, 1966).
cmdscale(d, k = 2, eig = FALSE, add = FALSE, x.ret = FALSE,
list. = eig  add  x.ret)
d 
a distance structure such as that returned by 
k 
the maximum dimension of the space which the data are to be
represented in; must be in 
eig 
indicates whether eigenvalues should be returned. 
add 
logical indicating if an additive constant 
x.ret 
indicates whether the doubly centred symmetric distance matrix should be returned. 
list. 
logical indicating if a 
Multidimensional scaling takes a set of dissimilarities and returns a set of points such that the distances between the points are approximately equal to the dissimilarities. (It is a major part of what ecologists call ‘ordination’.)
A set of Euclidean distances on n
points can be represented
exactly in at most n  1
dimensions. cmdscale
follows
the analysis of Mardia (1978), and returns the bestfitting
k
dimensional representation, where k
may be less than the
argument k
.
The representation is only determined up to location (cmdscale
takes the column means of the configuration to be at the origin),
rotations and reflections. The configuration returned is given in
principalcomponent axes, so the reflection chosen may differ between
R platforms (see prcomp
).
When add = TRUE
, a minimal additive constant c*
is
computed such that the dissimilarities d_{ij} + c*
are Euclidean and hence can be represented in n  1
dimensions. Whereas S (Becker et al, 1988) computes this
constant using an approximation suggested by Torgerson, R uses the
analytical solution of Cailliez (1983), see also Cox and Cox (2001).
Note that because of numerical errors the computed eigenvalues need
not all be nonnegative, and even theoretically the representation
could be in fewer than n  1
dimensions.
If .list
is false (as per default), a matrix with k
columns whose rows give the coordinates of the points chosen to
represent the dissimilarities.
Otherwise, a list
containing the following components.
points 
a matrix with up to 
eig 
the 
x 
the doubly centered distance matrix if 
ac 
the additive constant 
GOF 
a numeric vector of length 2, equal to say

Becker, R. A., Chambers, J. M. and Wilks, A. R. (1988). The New S Language. Wadsworth & Brooks/Cole.
Cailliez, F. (1983). The analytical solution of the additive constant problem. Psychometrika, 48, 343–349. doi:10.1007/BF02294026.
Cox, T. F. and Cox, M. A. A. (2001). Multidimensional Scaling. Second edition. Chapman and Hall.
Gower, J. C. (1966). Some distance properties of latent root and vector methods used in multivariate analysis. Biometrika, 53, 325–328. doi:10.2307/2333639.
Krzanowski, W. J. and Marriott, F. H. C. (1994). Multivariate Analysis. Part I. Distributions, Ordination and Inference. London: Edward Arnold. (Especially pp. 108–111.)
Mardia, K.V. (1978). Some properties of classical multidimensional scaling. Communications on Statistics – Theory and Methods, A7, 1233–41. doi:10.1080/03610927808827707
Mardia, K. V., Kent, J. T. and Bibby, J. M. (1979). Chapter 14 of Multivariate Analysis, London: Academic Press.
Seber, G. A. F. (1984). Multivariate Observations. New York: Wiley.
Torgerson, W. S. (1958). Theory and Methods of Scaling. New York: Wiley.
dist
.
isoMDS
and sammon
in package MASS provide alternative methods of
multidimensional scaling.
require(graphics)
loc < cmdscale(eurodist)
x < loc[, 1]
y < loc[, 2] # reflect so North is at the top
## note asp = 1, to ensure Euclidean distances are represented correctly
plot(x, y, type = "n", xlab = "", ylab = "", asp = 1, axes = FALSE,
main = "cmdscale(eurodist)")
text(x, y, rownames(loc), cex = 0.6)