Equatorwards western boundary currents occur in tropical and polar locations, e.g. the East Greenland and Labrador currents, in the Atlantic and the Oyashio.
Not exact matches
[Response: The classical (i.e. Stommel) theory of the subtropical gyre requires that the interior
equatorward (Sverdrup) transport that takes place everywhere but a narrow strip along the
western edge of the basin, precisely balance the poleward transport that takes place in a narrow boundary current along the
western edge of the basin.
Thus, the subtropical gyre circulation is a horizontal circulation with poleward mass transport along the
western boundary, and
equatorward transport everywhere east of that, and providing no net northward mass transport integrated across the basin (which is what Bryden et al have done).
• surface upwelling (of cold / cool water) at / off
western continental margins, driven by Coriolis effect on
equatorward currents;
The arid conditions found along the
western coasts of continents in subtropical latitudes are further enhanced by the influence of the
equatorward surface air flow on the ocean currents.
Thus a less active sun gives colder winters and cooler wetter summers in
Western Europe simply because a less active sun gives more meridional /
equatorward mid latitutude jets.
And
western intensification of warm - water currents produces entirely different precipitation levels compared to opposite coasts washed by
equatorward - bound cool currents.