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The Global Station Papa Array is a set of three moorings. With a distance between moorings approximately ten times that of the water depth, the array is able to collect data on the mesoscale variability. Unlike the design of the Global Irminger Sea Array, the Global Station Papa array does not have an OOI Surface Mooring.
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The Irminger Sea is a marginal sea of the North Atlantic Ocean. It is bordered to the west by southern Greenland , to the north by Iceland and the Denmark Strait , to the east by the Reykjanes Ridge (a northern part of the Mid-Atlantic Ridge ), and to the south by open waters of the North Atlantic.
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Both barotropic and baroclinic instabilities generate vorticity leading to eddies called Irminger Rings. Associated with the formation of IRs is an increase in Eddy Kinetic Energy (EKE). [3] IRs are not the only type of eddy spawned around the Labrador Sea. Convective events in the interior Labrador sea create steep density gradients.
The console can also be used to execute Magik code and to see the results. Compiled code is stored in a single file called an image file. Each image file holds the compiled byte-codes and the state of the session (for example variable values) when the image was last saved.
The effectiveness of loop interchange depends on and must be considered in light of the cache model used by the underlying hardware and the array model used by the compiler. In C programming language, array elements in the same row are stored consecutively in memory (a[1,1], a[1,2], a[1,3]) ‒ in row-major order.
The Irminger Current is a north Atlantic ocean current setting westward off the southwest coast of Iceland. It is composed of relatively warm and saline waters from the eastern North Atlantic that are fed by the North Atlantic Drift .