Thermohaline Circulation

Large-scale ocean circulation that is driven by global density gradients created by surface heat and freshwater fluxes.[1][2] The adjective thermohaline derives from thermo- referring to temperature and -haline referring to salt content, factors which together determine the density of sea water. Wind-driven surface currents (such as the Gulf Stream) travel polewards from the equatorial Atlantic Ocean, cooling en route, and eventually sinking at high latitudes (forming North Atlantic Deep Water). This dense water then flows into the ocean basins. While the bulk of it upwells in the Southern Ocean, the oldest waters (with a transit time of around 1600 years)[citation needed] upwell in the North Pacific.[3] Extensive mixing therefore takes place between the ocean basins, reducing differences between them and making the Earth's oceans a global system. On their journey, the water masses transport both energy (in the form of heat) and matter (solids, dissolved substances and gases) around the globe. As such, the state of the circulation has a large impact on the climate of the Earth...

http://encyclopedia.thefreedictionary.com/Thermohaline+circulation

Update: the "Permanent Polar Pack Ice" notation on the older Thermohaline map has to be changed, as the Arctic ice pack is no longer "permanent" and in fact has been decreasing in volume year-to-year

See:

http://svs.gsfc.nasa.gov/cgi-bin/details.cgi?aid=4251]

http://svs.gsfc.nasa.gov//vis/a000000/a004200/a004251/multiyear_ice_2014_no_graph_1080.mp4

https://upload.wikimedia.org/wikipedia/commons/thumb/2/2d/Ocean_currents_1943_for_colorblind_users.png/1920px-Ocean_currents_1943_for_colorblind_users.png