•Significant errors exist within the NAVD 88
•Similar magnitude errors could exist within
EGM96 or other EGM’s
•Future EGM’s will directly
impact the gravimetric geoid solutions at the long to intermediate
wavelengths
•Seamless gravity data is needed
from deep ocean onto shore and off the opposite national
coast(s) to resolve shorter wavelengths
•Resulting gravimetric models can
be studied in the context of MDT models to determine the best
fitting littoral geoid
•The implication then would be
that these models would also be suitable in the interior
•Such geoid models will better
resolve orthometric heights and provide an improved
relationship between oceanographic and terrestrial applications