The hyperbolic multiquadric method is defined by
n
GMG, y) = > ej v d, y)+r (2)
1=
where d; 2x, y) is given above, r must be specified,
and the coefficients c; are found by solving the n by
pi»Lb-,.n GMis
localized as follows: for each data point (xi, yi^
GM is determined by the nineteen points closest to
(xj, y) plus (x;, y) itself.
n system GM(x, y) - F
The weighted quadratic least squares method GQ
is determined by the ten points closest to G5, Y)
plus (x;, y;) itself, for each data point (xj, yj). The
weights are
wi%, ¥) = (1; - da, y? 3)
where r; equals the distance between Gu, y;) and
the most distant of the ten closest points. In
addition, the weighted planar least squares
method GP is determined by the eight points
closest to (xi, y;) plus Gu, yj) itself, for each data
point (x;, y;). The weights as above are used with
r; equal to the distance between (x, yj) and the
most distant of the eight closest points.
The triangular Shepard method is defined by the n
data (x, y; Filz and a triangulation (v1;,
v2, v3); 4, where m is the number of triangles
in the triangulation. It is given by
m
GT, y) 2 Y wj, y) LF;(x, y) (4)
i=l
where
1 1
w;(x, y) = 3 LN 2
2 izk 9
[la en [[ae»
j=1 j=1
LF;(x, y) is the linear interpolant over the i-th
triangle, and di is the Euclidean distance from (x,
y) to vertex j of the triangle i. Note that no
parameters need be specified for LF, although it is
dependent on the triangulation.
930
4. SURFACE INTERPOLANTS
Several interpolation schemes that assume
prescribed values and their gradients on the
boundary of a planar triangle have been
developed. Barnhill, Birkhoff, and Gordon (1973)
first developed such a method using lines parallel
to the triangle sides, and Nielson (1979) has
developed method for line segments joining
vertices to their opposite sides. This method
consists of using the planar interpolant on the
underlying planar triangle with boundary data
obtained by projecting values and gradients onto
the plane.
For such an interpolation, let p be a point of the
triangle with vertices, in counterclockwise order
v1, v2, and v3, and let p' be the central projection of
p onto the underlying planar triangle having the
same vertices T - (v1,v2,v3), i.e., boundary points
of the triangle project to boundary points of T.
Denote by bl, b2, and b3 the barycentric
coordinates of p' with respect to T. These are
defined by
3
EE (5)
1=1
and
3
Y bi Vi = p (6)
i=l
This is a basic scheme of piecewise linear surface
interpolation. This scheme is given a
triangulation of a set of points in the plane and
computes the value at (x, y) of a piecewise linear
surface. Equivalently, b; = A;/A, where A is the
area of t and A; is the area of the subtriangle (p',
vi VE) for (i, j, ke s = {(1,2,3), (2,3,1), (3,1,2)).
Consider the line defined by v1 and p'. This line
intersects the edge opposite v1 at the point
_b2v2+b3v3
qu=-""2+h3 (7)
The points q2' and q3' lying on the sides opposite
v2 and v3, respectively, are defined similarly. The
following side-vertex-based interpolant is derived
by Lawson (1977). For a bivariate function f on T,
the interpolant defines
3
F(p) » Y, w; Hp) (8)
i=1