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dc.contributor.authorSadler, James
dc.date.accessioned2010-01-15T00:50:54Z
dc.date.available2010-01-15T00:50:54Z
dc.date.issued2010-01-15T00:50:54Z
dc.identifier.urihttp://hdl.handle.net/1773/15570
dc.descriptionSenior thesis written for Oceanography 444en_US
dc.description.abstractCTD-O, light backscatter and oxidation-reduction potential data were obtained for the hydrothermal plumes of the Brothers volcano. The data was compared to 2002 and 2007 datasets. Taken together, the data indicate that the plume is being advected in a westerly direction. Turbidity decreased significantly from 2002 to 2009. Other trends are discussed.en_US
dc.language.isoen_USen_US
dc.subjectVolcanic plumes--South Pacific Ocean--Kermadec Arcen_US
dc.subjectBrothers volcano--South Pacific Ocean--Kermadec Arcen_US
dc.subjectSalinity--South Pacific Ocean--Kermadec Arc--Observationsen_US
dc.subjectChemical oceanography--South Pacific Ocean--Kermadec Arc--Observationsen_US
dc.titleTemporal changes in venting at Brothers volcano, as indicated by backscatter and oxidation-reduction potentialen_US
dc.typeOtheren_US


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