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An inverse model to infer the near-surface velocity from the heat equation was applied to a series of six infrared satellite images from northern California. The inversion used a two-dimensional nondi...
A nonlinear finite-difference inverse model is used for estimating the North Atlantic general circulation between 20° and 50°N. The inverse model with grid spacing 2° latitude and 2.5° longitude is ba...
An inverse model was developed of the seasonal upper-layer circulation in the region adjacent to the coast of southern Brazil between 30° and 35°S, 50° and 55°W near the boundary of the Brazil–Malvina...

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