H040-0016
Variational Analysis to reconstruct the 3D dynamics of an anticyclonic eddy, possible use of SWOT observations.
Abstract:
This method uses the ADCP velocities and the thermal wind balance to avoid an artificial curvature of the isopycnal when reconstructing the density field from uCTD. The shape of the reconstructed features is important when, as in this case, the vertical velocity is calculated through the QG and SG omega equations. Drifter trajectories have been used to evaluate the improvements of this reconstruction method compared to the OI.
The along-isopycnal component of the vertical velocity has also been estimated by projecting the non-divergent component of the ADCP velocities to an isopycnal surface. These three different estimations of the vertical velocity field from observational data provide an advance in understanding the dynamics associated with mesoscale features. Indirect validation of these vertical velocity fields has been observed in the biological samples from CTD casts which present subduction evidence in agreement with the negative values of w.
The available altimeters were helpful to locate the eddy during the cruise planning but had limitations in defining its shape due to the lack of resolution, which confirms the need for the SWOT high-resolution observations. The role of the ADCP data in the multivariate analysis used in this study can be in the future played by the horizontal velocities derived from SWOT observations. The combination of a multivariate reconstruction method with the SWOT observations can thus provide a better estimation of nutrients fluxes and heat transport can on global scales.