Interpolation and gridding of data are procedures in the physical scie
nces and al-e accomplished typically using an averaging or finite diff
erence scheme on an equidistant grid. Cubic splines are popular becaus
e of their smooth appearances; however, these functions can have undes
irable oscillations between data points. Adding tension to the spline
overcomes this deficiency. Here, we derive a technique for interpolati
on and gridding in one, two, and three dimensions using Green's functi
ons for splines in tension and examine some of the properties of these
functions. For moderate amounts of data, the Green's function techniq
ue is superior to conventional finite-difference methods because (1) b
oth data values and directional gradients can be used to constrain the
model surface, (2) noise can be suppressed easily by seeking a least-
squares fit rather than exact interpolation, and (3) the model can be
evaluated at arbitrary locations rather than only on a rectangular gri
d. We also show that the inclusion of tension greatly improves the sta
bility of the method relative to gridding without tension. Moreover, t
he one-dimensional situation can be extended easily to handle parametr
ic curve fitting in the plane and in space. Finally, we demonstrate th
e new method on both synthetic and real data and discuss the merits an
d drawbacks of the Green's function technique.