Pietri A. auteur aut IRD Capet X. auteur aut IRD D'Ovidio F. auteur aut IRD Levy Marina auteur aut IRD Le Sommer J. auteur aut IRD Molines J. M. auteur aut IRD Giordani H. auteur aut IRD text journalArticle eng text/pdf born digital access The quasigeostrophic and the generalized omega equations are the most widely used methods to reconstruct vertical velocity w from in situ data. As observational networks with much higher spatial and temporal resolutions are being designed, the question arises of identifying the approximations and scales at which an accurate estimation of w through the omega equation can be achieved and what critical scales and observables are needed. In this paper we test different adiabatic omega reconstructions of w over several regions representative of main oceanic regimes of the global ocean in a fully eddy-resolving numerical simulation with a 1/60 degrees horizontal resolution. We find that the best reconstructions are observed in conditions characterized by energetic turbulence and/or weak stratification where near-surface frontal processes are felt deep into the ocean interior. The quasigeostrophic omega equation gives satisfactory results for scales larger than similar to 10 km horizontally while the improvements using a generalized formulation are substantial only in conditions where frontal turbulent processes are important (providing improvements with satisfactory reconstruction skill down to similar to 5 km in scale). The main sources of uncertainties that could be identified are related to processes responsible for ocean thermal wind imbalance (TWI), which is particularly difficult to account for (especially in observation-based studies) and to the deep flow that is generally improperly accounted for in omega reconstructions through the bottom boundary condition. Nevertheless, the reconstruction of mesoscale vertical velocities may be sufficient to estimate vertical fluxes of oceanic properties in many cases of practical interest. specialized Ageostrophic circulations Fluxes Mesoscale processes Vertical motion 032 020 51 3 931-954 2021 0022-3670 https://www.documentation.ird.fr/hor/fdi:010081504 10.1175/jpo-d-20-0052.1 0022-3670 [F B010081504] https://www.documentation.ird.fr/hor/fdi:010081504 https://www.documentation.ird.fr/intranet/publi/2021-07/010081504.pdf Accès réservé (Intranet de l'IRD) IRD - Base Horizon / Pleins textes 2021-07-02 2025-02-24 fdi:010081504 fre