Positive+and+negative+feedbacks+related+to+the+Arctic+Oscillation+revealed+by+air+sea+heat+fluxes.pdf (3.132Mb)

Simulated northward, southward, and net northward (northward-southward) volume (Sv), heat flow (TW) and fresh water flux (0.01 Sv) through the Denmark Strait (DS), across

The Arctic upper ocean and sea ice cover receives net heat input in summer, as shortwave radiation and sensible heat fluxes directly heat the sea ice (including its snow layer),

Heat transfer coefficient and pressure drop were determined at saturation temperatures 0, 5 and 10 °C for the smooth tube, while the three tubes were compared at heat fluxes

• In contrast, models with a positive correlation be- tween the heat transport into the Nordic Seas and the Subpolar Gyre Index have a weaker heat trans- port than expected from

My main findings are that there is an enhanced low-frequency variability in the North Atlantic, that both the ocean heat transport divergence and the surface heat flux play an

Figure 2.9: Schematic diagram showing the Arctic Ocean (shelves and basins) and key pro- cesses that affect the oceanic heat fluxes and hence the sea ice. 1-5 illustrates

The interannual variability in convection depth through the record depended on heat loss to the atmosphere, the stratification of the water column, and lateral fluxes of heat

The content method gave larger estimates, and during current experiments the sign followed what was expected for both heat and salt fluxes (cf Figure 2.3), except the heat flux