Abyssal gyres

The flow of Antarctic Bottom Water in the western part of the Atlantic Ocean is modeled in terms of an annulus consisting of a coupled frontal current (i.e., a cold filament) moving along the internal surface of a cone. Namely, the interface bounding the (reduced-gravity) cyclonic current from above...

Ausführliche Beschreibung

Bibliographische Detailangaben

Veröffentlicht in:	Geophysical and astrophysical fluid dynamics 1991-07, Vol.58 (1-4), p.173-196
Hauptverfasser:	Nof, Doron, Paldor, Nathan, Gorder, Stephen Van
Format:	Artikel
Sprache:	eng
Schlagworte:	Antarctic Coriolis parameter Dynamics of the ocean (upper and deep oceans) Earth, ocean, space Exact sciences and technology External geophysics Physics of the oceans Rossby number
Online-Zugang:	Volltext
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