Interaction of the North Atlantic current with the deep Charlie Gibbs Fracture Zone throughflow

Rez.: The Charlie Gibbs Fracture Zone (CGFZ), a passage of 3600 m sill depth through the Mid-Atlantic Ridge near 52°N, is a knwon gateway for the passage of deep waters from the Northeast Atlantic into the western basin. During a shipboard survey of August 1997 deep current profiling yielded eastwar...

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Veröffentlicht in:Geophysical research letters
1. Verfasser: Schott, Friedrich A. (VerfasserIn)
Weitere Verfasser: Stramma, Lothar (VerfasserIn), Fischer, Jürgen (VerfasserIn)
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Sprache:eng
Veröffentlicht: 1999
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