This study focuses on the improved estimation of mesoscale surface ocean ci
rculation obtained by merging TOPEX/Poseidon (T/P) and ERS-1 and -2 altimet
er measurements between October 1992 and May 1998. Once carefully intercali
brated and homogenized, these data are merged through an advanced global ob
jective analysis method that allows us to correct for residual long wavelen
gth errors and uses realistic correlation scales of ocean dynamics, The hig
h-resolution (0.25 degrees x 0.25 degrees) merged T/P + ERS-1 and -2 sea le
vel anomaly maps provide more homogeneous and reduced mapping errors than e
ither individual data set and more realistic sea level and geostrophic velo
city statistics than T/P data alone. Furthermore, the merged T/P + ERS-1 an
d -2 maps yield eddy kinetic energy (EKE) levels 30% higher than maps of T/
P alone. They also permit realistic global estimates of east and north comp
onents of EKE and their seasonal variations, to study EKE sources better. A
comparison of velocity statistics with World Ocean Circulation Experiment
surface drifters in the North Atlantic shows very good agreement. Compariso
n with contemporary current meter data in various oceanic regimes also prod
uces comparable levels of energy and similar ratios of northward and eastwa
rd energy, showing that the maps are suitable to studying anisotropy. The T
/P + ERS zonal and meridional components of the mapped currents usually pre
sent comparable rms variability, even though the variability in the Atlanti
c is more isotropic than that in the Pacific, which exhibits strong zonal c
hanges. The EKE map presents a very detailed description, presumably never
before achieved at a global scale. Pronounced seasonal changes of the EKE a
re found in many regions, notably the northeastern Pacific, the northeaster
n and northwestern Atlantic, the tropical oceans, and the zonally extended
bands centered near 20 degrees S in the Indian and western Pacific Oceans a
nd at 20 degrees N in the northwestern nl Pacific.