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.
机构:
Univ Siegen, Res Inst Water & Environm, Paul Bonatz Str 9-11, D-57076 Siegen, GermanyUniv Siegen, Res Inst Water & Environm, Paul Bonatz Str 9-11, D-57076 Siegen, Germany