Importance of ice‐ocean interactions for the global ocean circulation: A model study

Abstract

Abstract. Numerical experiments are conducted with a coarse-resolution global ice-ocean model in order to determine to what degree the sea ice-ocean exchanges of heat, salt/freshwater, and momentum control the general circulation of the world ocean on long timescales. These experiments reveal that the formation of North Atlantic Deep Water (NADW) in the model results from the strong heat losses that occur at the oceanic surface in the high-latitude North Atlantic. The large-scale ice-ocean interactions have nearly no influence on this process. In particular, neglecting the fYeshwater flux associated with the southward ice transport at Fram Strait does not impact seriously on the salinity of the Greenland and Norwegian Seas. At equilibrium the absence of this freshwater flux is balanced by an enhanced oceanic freshwater transport from the Arctic. Furthermore, it appears that the model NADW formation does not critically depend on the media (ice or ocean) transporting the freshwater. Besides, both the salt/freshwater and heat exchanges between sea ice and ocean are crucial in the Southern Ocean for the deep water production, properties, and export. The large amount of brine released during ice formation on the model Antarctic continental shelf leads to very high salinities there. The resulting dense shelf waters are then transported toward great depths after some mixing with ambient waters, finally forming the Antarctic Bottom Water body. On the other hand, the net ice melting associated with ice convergence in some areas, such as the southwestern Pacific, stabilizes the water column and forbids deep mixing in these regions. Furthermore, the contact with the ice imposes that the polar surface waters must be maintained very close to their tYeezing point temperature. Our results suggest that this process takes an important part in increasing the density of the Antarctic Bottom Water. We also show that the modifications of the stress at the ocean surface induced by the internal ice stress have only a regional effect.

Future discharge drought across climate regions around the world modelled with a synthetic hydrological modelling approach forced by three general circulation models

“…Through the EU-WATCH project, simulation outcome from three GCMs was available on a global scale. The GCMs included are ECHAM5 (Roeckner et al, 2003;Jungclaus et al, 2006), CNRM3 (Royer et al, 2002;Salas-Mélia, 2002) and IPSL (Hourdin et al, 2006;Madec et al, 1998;Fichefet and Maqueda, 1997;Goosse and Fichefet, 1999). Each GCM provides meteorological forcing for the period 1960-2100.…”

“…WATCH cells) were randomly selected around the world. The Köppen-Geiger climate classification (Köppen, 1900;Geiger, 1954Geiger, , 1961) was used to ensure that sufficient locations were selected in all different major climate regions. The five climate types distinguished in this study are: Equatorial (A), Arid (B), Warm temperate (C), Snow (D) and Polar climates (E).…”

Simulation of the Global Hydrological Cycle in the CCSM Community Atmosphere Model Version 3 (CAM3): Mean Features

“…When sea ice dynam-ics are considered, the transport of relatively fresh sea ice redistributes water in the system, influencing the global hydrological cycle. This has the potential to modify the large scale ocean circulation in both the southern (e.g., Goosse and Fichefet 1999) and the northern (e.g., Holland et al 2001) hemispheres.…”

Deglacial ice sheet meltdown: orbital pacemaking and CO<sub>2</sub> effects

“…4. The ocean-sea ice component of LOVECLIM, CLIO (Goosse and Fichefet, 1999, Coupled Large-scale Ice Ocean), computes ocean currents, salinity, and temperature according to the primitive equations on two spherical subgrids covering the global oceans at a resolution of 3 • by 3 • horizontally, and 20 levels vertically; sea ice thermodynamics and advection are computed on the same horizontal grid.…”