in

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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Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Kerguelen
Kerguelen Islands
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
id ftciteseerx:oai:CiteSeerX.psu:10.1.1.486.9166
record_format openpolar
spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.486.9166 2023-05-15T17:02:00+02:00 in The Pennsylvania State University CiteSeerX Archives application/pdf 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 en eng 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 Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.noc.soton.ac.uk/soes/staff/acng/DSRII_Parketal08.pdf text ftciteseerx 2016-01-08T08:14:57Z 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 Text Kerguelen Islands Unknown Kerguelen Kerguelen Islands
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description 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
author2 The Pennsylvania State University CiteSeerX Archives
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url 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
geographic Kerguelen
Kerguelen Islands
geographic_facet Kerguelen
Kerguelen Islands
genre Kerguelen Islands
genre_facet Kerguelen Islands
op_source http://www.noc.soton.ac.uk/soes/staff/acng/DSRII_Parketal08.pdf
op_relation 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
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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