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GROGRAT
is a four-dimensional ray-tracing algorithm which can
accurately trace nonhydrostatic gravity waves through any gridded numerical
representation of the Earth's neutral atmosphere. The first version (V1.0) of
this model was described by Marks
and Eckermann (1995). Recent updates of the code and results of some
test experiments with newer versions of the code have been reported
recently by Eckermann and Marks (1997).
New features
from version 1.0 include updated infra-red radiative damping parameterizations,
full 4D interpolation of background fields, provision for a background vertical velocity
field, automatic internal conversion of fields from
pressure or log-pressure gridding to geometrical height grids, refraction
due to time-varying flow fields, interfaces of the FORTRAN code for C and
IDL applications, and accommodation of either forward (upwards) or backward
(downwards) ray-tracing experiments.