Figure 10: Conceptual illustration of the Atlantic con
veyor
circulation. High salinity water is chilled and sinks in the far
North Atlantic, promoting a compensating northward surface layer flow
of warm, high salinity water (after Broecker 1991). Important
components of the southern circumpolar circulations, represented by
the dashed lines, have been added to Broecker's original figure (see
text). The area labeled ``IT" just northwest of Australia specifies
the ``Indonesian Throughflow``. The encircled numbers represent
estimated long term mean values for upper-level current flux into the
South Atlantic Ocean in Sverdrups (Sv =3D 106 m3/s) from the
South Pacific (10 Sv) and from the South Indian Ocean (4 Sv) which
are entrained into the northward moving upper layer circulation of
the South Atlantic.