Ocean angular momentum (OAM) calculations using forward model runs without
any data, constraints have recently revealed the effects of OAM variability
on the Earth's rotation. Here we use an ocean model and its adjoint to est
imate OAM values bg constraining the model to available oceanic data. The o
ptimization procedure yields substantial changes in OAM, related to adjustm
ents in both motion and mass fields. as well as in the wind stress torques
acting on the ocean. Constrained and unconstrained OAM values are discussed
in the contest of closing the planet's angular momentum budget. The estima
tion procedure yields noticeable improvements in the agreement with the obs
erved Earth rotation parameters, particularly at the seasonal timescale. Th
e comparison with Earth rotation measurements provides an independent consi
stency check on the estimated ocean state and underlines the importance of
ocean state estimation for quantitative studies of the variable large-scale
oceanic mass and circulation fields, including studies of OAM.