Northward ocean heat transport achieved by the AMOC is responsible for the relative warmth of the Northern Hemisphere, compared to the Southern Hemisphere, and is thought to play a role in setting the mean position of the Inter-Tropical Convergence Zone north of the equator.
Not exact matches
All of these characteristics (except for the
ocean temperature) have been used in SAR and TAR IPCC (Houghton et al. 1996; 2001) reports for model - data inter-comparison: we considered as tolerable the following intervals for the annual means of the following climate characteristics which encompass corresponding empirical estimates: global SAT 13.1 — 14.1 °C (Jones et al. 1999); area of sea ice in the Northern Hemisphere 6 — 14 mil km2 and in the Southern Hemisphere 6 — 18 mil km2 (Cavalieri et al. 2003); total precipitation rate 2.45 — 3.05 mm / day (Legates 1995); maximum Atlantic
northward heat transport 0.5 — 1.5 PW (Ganachaud and Wunsch 2003); maximum of North Atlantic meridional overturning stream function 15 — 25 Sv (Talley et al. 2003), volume averaged
ocean temperature 3 — 5 °C (Levitus 1982).
While the circulation of the Atlantic
Ocean has a complex three - dimensional spatial structure, the zonally integrated flow in the basin, referred to as the Atlantic Meridional Overturning Circulation (AMOC), is largely responsible for the net
northward oceanic
heat transport on climate - relevant timescales.
Heat from anomalously warm
ocean temperatures is
transported vertically and eventually
northward by unusually active tropical convection (thunderstorms), warming the upper atmosphere in the lower latitudes.
Temperatures in the neighboring deep
ocean are moderated by strong
northward transport of
heat in the Gulf Stream, which begins to veer eastward before reaching Georges Bank.