EO·Atlas
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Ocean currents covers surface and upper-ocean circulation: the direction and speed of water movement that affects routing, search and rescue, pollutant drift, ecosystem transport, and climate variability. In satellite workflows the current is usually not observed as a visible object. It is estimated from sea-surface height gradients, wind forcing, sea-surface temperature structure, and model or in-situ constraints.[1][2]

For basin-scale circulation, radar altimetry is the primary EO route because sea-surface-height gradients constrain geostrophic flow. Operational products then fuse altimetry with SST, winds, in-situ observations, and model physics to produce gridded surface or 3D velocity fields.[1][3]

SAR products can add local ocean context through wind, swell, and radial-velocity variables.[4]

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4 Data products
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How to cite this page

Plain text

Ocean currents. EO-Atlas, SpectraWorks B.V. https://eo-atlas.org/topics/ocean-currents (CC BY 4.0)

BibTeX

@misc{eoatlas:topics:ocean-currents,
  title = {Ocean currents},
  author = {{EO-Atlas}},
  publisher = {SpectraWorks B.V.},
  note = {CC BY 4.0},
  url = {https://eo-atlas.org/topics/ocean-currents}
}