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Riding the Canary deep poleward undercurrent

descriptionPublicationkeyboard_double_arrow_right Conference object 11 Jun 2014 Spain English Publisher:Centro Oceanográfico de Canarias
Authors: Vélez-Belchí, P. (Pedro); Hernández-Guerra, A. (Alonso); González-Pola, C. (César); Machín, F.; Collins, C.;

handle: 10261/318073 , 10508/2651

Riding the Canary deep poleward undercurrent

Abstract

Poleward undercurrents are well known features in Eastern Boundary systems. In the California up- welling system (CalCEBS), the poleward flow has been observed along the entire outer continental shelf and upper-slope, (1000m) than the poleward flow in the CalCEBS (<500m). The differences are explored based on the hypothesis that then gradient between the Mediterranean Outflow Waters and the Antartic Intermediate Waters contribute to force the deep flow in the CalCEBS.

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Spain
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Centro Oceanográfico de Canarias, Medio Marino

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selected citations
These citations are derived from selected sources.
This is an alternative to the "Influence" indicator, which also reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically).
BIP!Citations provided by BIP!
popularity
This indicator reflects the "current" impact/attention (the "hype") of an article in the research community at large, based on the underlying citation network.
BIP!Popularity provided by BIP!
influence
This indicator reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically).
BIP!Influence provided by BIP!
impulse
This indicator reflects the initial momentum of an article directly after its publication, based on the underlying citation network.
BIP!Impulse provided by BIP!
views
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European Marine Science