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- W2083579897 abstract "A combination of horizontally propagating plane waves were fitted to observations of mid-ocean mesoscale eddies from the Mid-Ocean Dynamics (MODE-0 and MODE-I) Experiments. The former included only current meter measurements, most from beneath and main thermocline. The latter much larger data set-from current meters, moored temperature sensors, hydrographic stations, and float tracks-gave a more uniform depth distribution. The plane waves were solutions of the linearized equation for the conservation of quasi-geostrophic potential vorticity. The free parameters of the wave model were optimally chosen to minimize an error norm for the differences between the observations and the wave fit. The wave fits were judged to be successful, having high correlations with the data (0·7) and accounting for a considerable fraction of the observed signal (70% r.m.s.). The model vertical structure involved both the barotropic and first baroclinic modes. The observed temporal evolution was generally consistent with the propagation predicted by the wave dispersion relation. Separate wave fits to the velocity and density observations were similar, which indicates their compatibility with the geostrophic thermal wind relation. Non-linear interactions within the wave fits were found to be weak for MODE-0 and of marginal (but uncertain) importance for MODE-I." @default.
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- W2083579897 date "1976-04-01" @default.
- W2083579897 modified "2023-10-04" @default.
- W2083579897 title "Optimal, quasi-geostrophic wave analyses of MODE array data" @default.
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- W2083579897 doi "https://doi.org/10.1016/0011-7471(76)90871-8" @default.
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