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dc.contributor.authorBoyd, P.en_US
dc.contributor.authorMcTainsh, Granten_US
dc.contributor.authorSherlock, V.en_US
dc.contributor.authorRichardson, K.en_US
dc.contributor.authorNichol, S.en_US
dc.contributor.authorEllwood, M.en_US
dc.contributor.authorFrew, R.en_US
dc.date.accessioned2017-04-24T08:15:34Z
dc.date.available2017-04-24T08:15:34Z
dc.date.issued2004en_US
dc.date.modified2009-10-01T05:52:43Z
dc.identifier.issn0886-6236en_US
dc.identifier.doi10.1029/2002GB002020en_AU
dc.identifier.urihttp://hdl.handle.net/10072/5209
dc.description.abstractAround 30% of oceanic waters are high nitrate low chlorophyll (HNLC) where low iron levels limit algal growth. HNLC waters have mainly been studied using shipboard and lab experiments. Since 1997, remote-sensing of phytoplankton via SeaWiFS Ocean Color has permitted monitoring of the constancy of this "HNLC condition," i.e., spatial homogeneity and low temporal variability of chlorophyll over annual cycles. These trends can be exploited, as episodic iron inputs should be conspicuous by subsequent expression as iron-elevated algal stocks. Subantarctic (SA) waters near New Zealand are HNLC, and the proximity of the arid Australian landmass, and the iron-rich Subtropical Front, provide natural laboratories to detect episodic atmospheric and oceanic iron supply, respectively. Two approaches were used: Oceanic supply was inferred from episodic increases in chlorophyll concentrations in SA waters, detected using Ocean Color archives. Additional archives were used to confirm the oceanic provenance of iron supply, and identify supply mechanism(s). Atmospheric supply was assessed using data on source areas and loads for dust storms monitored in central Australia. Dust transport and its fate was assessed using air mass forward trajectories and SeaWiFS Ocean Color and Aerosol Optical Depth maps. During 1997-2001, episodic elevated chlorophyll events occurred in SA waters southeast of New Zealand. There was no evidence of these events being mediated by atmospheric iron supply; however, neither wind-driven lateral advection or vertical mixing alone could account for these episodes. Dust storms, over this period sent plumes either into high iron SubTropical (ST) waters or into SA waters in early spring, when cells are probably light- rather than iron-limited.en_US
dc.description.peerreviewedYesen_US
dc.description.publicationstatusYesen_AU
dc.languageEnglishen_US
dc.language.isoen_AU
dc.publisherWiley-Blackwell Publishingen_US
dc.publisher.placeUnited Statesen_US
dc.publisher.urihttp://www.agu.org/journals/gb/en_AU
dc.relation.ispartofpagefrom1en_US
dc.relation.ispartofpageto23en_US
dc.relation.ispartofissue1en_US
dc.relation.ispartofjournalGlobal Biogeochemical Cyclesen_US
dc.relation.ispartofvolume18en_US
dc.subject.fieldofresearchcode260401en_US
dc.titleEpisodic enhancement of phytoplankton stocks in New Zealand subantarctic waters: contribution of atmospheric and oceanic iron supplyen_US
dc.typeJournal articleen_US
dc.type.descriptionC1 - Peer Reviewed (HERDC)en_US
dc.type.codeC - Journal Articlesen_US
gro.date.issued2004
gro.hasfulltextNo Full Text


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