
Physical Oceanographer at the Netherlands Institute for Sea Research (NIOZ). I am a human as well as a scientist. Views my own. @fmkdejong@fediscience.org
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ALT Vertical-latitude sections of salinity in the Atlantic (top) and Pacific (bottom). In the Atlantic, you can see the deep penetration of northern origin waters to 2000-3000m, from which we infer southward flow. In the Pacific, no such connection exists from the surface at northern latitudes to the mid-depth.

ALT Schematic representation of circulation in the Atlantic where the Gulf Stream (along the east coast of the USA, flowing northwards) splits somewhere offshore of the Atlantic, with one 'branch' flowing northwards as part of the AMOC and the other branch flowing southwards as part of the return circulation of the subtropical gyre.

ALT Map of the Atlantic from Antarctica to the Arctic, showing bathymetry in the ocean basins, and contours of dynamic topography. Overlaid are sketched arrows showing clockwise circulation in the northern subtropical gyre and Weddell gyre, and counter clockwise in the southern subtropical gyre and northern subpolar gyre.















