The upper panel illustrates how ENSO influences the equatorial Atlantic and Indian Oceans, and how these two ocean basins in turn feed back to ENSO. On the right side of the panel, the schematic shows ...
The movement of water masses in the ocean, its circulation, is an essential component of the global climate system. Researchers have now been able to show that circulation in the deep ocean was ...
This is a preview. Log in through your library . Abstract The Stommel and Arons model of the circulation in the abyssal ocean is modified by allowing the temperature (homogeneous in Stommel-Arons) to ...
The oceanic mesoscale, 10–100 km, is the equivalent of the atmospheric storm scale. It is generally considered to be the most energetic scale, and it is where fronts between water masses become ...
This is a preview. Log in through your library . Abstract ABSTRACT On the basis of the multidecadal component of a Fram Strait sea ice export reconstruction and on a sea surface temperature proxy for ...
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