Analyzing contributions of atmospheric forced variability versus the oceanic intrinsic variability for sea level observations
As the atmospheric evolution may force a variety of long-term oceanic variability, this means that the most accurate satellite/in situ observations can describe the atmospheric forced variability along with the chaotic ocean intrinsic changes. The OVALIE project proposes to scientifically investigate and partition the respective contribution of the atmospheric forced variability versus the oceanic intrinsic variability for the sea level observations (satellite data -based on Topex/Poseidon, Jason 1-2-3, ERS1, ERS2, ENVISAT, Altika and GRACE- and in situ measurements –based on Argo floats and other in situ measurements).