As part of the European AGORA programme we have been assimilating TOPEX/POS
EIDON altimeter data into the Southampton Oceanography Centre's high resolu
tion (1/4 degree, 36 level) global ocean model (OCCAM). The assimilation me
thod used is that of Cooper and Haines, a dynamically based method which co
nserves water properties on isopycnal surfaces. Results of a one-year, 1993
, run of this model, driven by ECMWF B-hourly winds and assimilating 10-day
mapped TOPEX/POSEIDON data are presented. A method to improve the model me
an sea level for use in altimeter assimilation is described and implemented
in the Gulf Stream and Kuroshio separation regions. Results demonstrate th
e model's ability to adjust to this new mean sea surface and to also propag
ate the assimilated altimeter signal realistically in time, an essential ch
aracteristic if ocean forecasting is to be attempted. (C) 1999 Elsevier Sci
ence Ltd. All rights reserved.