We have calculated fundamental and overtone OH-stretching vibrational band
intensities of the water dimer and trimer. The intensities were determined
with a simple harmonically coupled anharmonic oscillator (HCAO) local mode
model and ab initio dipole moment functions. The dipole moment functions we
re calculated at the self-consistent-field Hartree-Fock and quadratic confi
guration interaction including single and double excitations levels of theo
ry with the 6-31G(d), 6-311+G(d, p), and 6-311++G(2d, 2p) basis sets. The o
vertone spectra of the dimer and trimer have not been observed and a method
of obtaining local mode parameters from scaled ab initio calculations has
been suggested. We find that the falloff in absolute intensity with increas
ing overtone of the dimer and trimer is similar to the falloff observed for
the monomer. Our calculations show that the total overtone intensity of th
e dimer and trimer, although distributed differently, is close to two and t
hree times the total intensity of the monomer for a given region. One signi
ficant difference between the monomer and the dimer and trimer is the appea
rance of the red shifted hydrogen bonded OH-stretching band in the dimer an
d trimer spectra. We suggest that these red shifted bands are ideal for att
empts to observe the water dimer in the atmosphere. The method presented ca
n provide an accurate estimate of the OH-stretching intensities for molecul
es for which vibrational spectra have not been observed. Such calculations
are of importance in atmospheric solar energy absorption models. (C) 1999 A
merican Institute of Physics. [S0021-9606(99)00317-7].