This paper describes first steps towards the quasi-operational assimilation
of sea level anomalies from the TOPEX/POSEIDON and ERS1/2 missions into a
global ocean model that is used to initialize a coupled ocean-atmosphere se
asonal forecast system. We estimate the impact that assimilation of sea lev
el might have on the ocean analysis compared to the assimilation of subsurf
ace temperature observations. As a first step satellite-observed sea level
anomalies are compared with simulated sea level anomalies from model experi
ments. To assess the quality of the ocean analysis and the altimeter data f
urther, model results and satellite data are compared to independent sea le
vel observations from tide gauges. Model results are from three experiments
: no assimilation, assimilation of subsurface temperature data, and assimil
ation of sea level data, respectively. The comparison is focused on the equ
atorial Pacific where subsurface temperatures are frequently sampled and im
pact of subsurface oceanic conditions on forecast skill is assumed to be la
rge. It is shown that altimeter data assimilation can match subsurface temp
erature assimilation in this area. (C) 1999 Elsevier Science Ltd. All right
s reserved.