Reorganization of Miocene deep water circulation in response to the shoaling of the Central American Seaway

This report documents the experiences and lessons from the deployment of operational analysts to Afghanistan with the Norwegian Armed Forces, with regard to the concept, the main

Continuous arrows indicate flow of Modified North Atlantic Water (MNAW) and North Atlantic Water (NAW) in the upper layers (red), the cold Norwegian Seas Deep Water (NSDW) (purple),

In the model, these variations are caused by changes in the relative influence of North Atlantic Deep Water (NADW) and southern source water (SSW) and are closely linked to large

Comparison of CaCO 3 results with those from ODP Site 1089 and an index of North Atlantic Deep Water (NADW) influence in surface waters indicate that NADW upwelled along

Thermohaline circulation consists of various components resulting in deep global oceanic overturning including cooling of water (buoyancy loss) in the northern high

• To first order, the large scale ocean circulation response to an increase in the Arc- tic river runoff – slowdown of the Atlantic Meridional Overturning Circulation and the

In the model, these variations are caused by changes in the relative influence of North Atlantic Deep Water (NADW) and southern source water (SSW) and are closely linked to large

The sensitivity of the ocean circulation to changes in solar irradiance is examined using an isopycnic coordinate, global ocean general circulation model (OGCM) coupled to