The Atlantic meridional overturning circulation delivers warmth to high latitudes and carbon to depth. Historical temperature and salinity records call into question the traditional view that these waters form a single coherent conveyer system of currents.
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Univ Calif Santa Barbara, Earth Res Inst, Santa Barbara, CA 93106 USA
Univ Calif Santa Barbara, Dept Geog, Santa Barbara, CA 93106 USAUniv Calif Santa Barbara, Earth Res Inst, Santa Barbara, CA 93106 USA
Siegel, David A.
Franz, Bryan A.
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NASA, Ocean Biol Proc Grp, Goddard Space Flight Ctr, Greenbelt, MD 20771 USAUniv Calif Santa Barbara, Earth Res Inst, Santa Barbara, CA 93106 USA