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be men Par de phy Dec ine The major objective of the physical component of the region is found over the shallow shelf (o200m) north of the Kerguelen Islands and the other over the shallow plateau (o500m) south of the islands. The two areas are Polar Front (PF) skirting the southern edge of the islan...
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| Language: | English |
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.486.9166 http://www.noc.soton.ac.uk/soes/staff/acng/DSRII_Parketal08.pdf |
| Summary: | be men Par de phy Dec ine The major objective of the physical component of the region is found over the shallow shelf (o200m) north of the Kerguelen Islands and the other over the shallow plateau (o500m) south of the islands. The two areas are Polar Front (PF) skirting the southern edge of the islands important considering the general northward geostrophic flow in the area (Roquet et al., 2008; Park et al., 2008) and the presence of the PF possibly blocking any south-ARTICLE IN PRESSward penetration of lithogenic inputs of Kerguelen Islands origin. Therefore, our working hypothesis for KEOPS is that the iron in the surface layer originates |
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