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dc.contributor.authorHelman, Dan
dc.date.accessioned2008-07-23T18:03:01Z
dc.date.available2008-07-23T18:03:01Z
dc.date.issued2008-06-19
dc.identifier.citationKeil R., Kelley D., D'Asaro E., Krembs C., and Collins R.E. [Eds.] 2008. Proceedings from the University of Washington School of Oceanography Undergraduate Thesis Research Expedition to Glacier Bay Alaska, March 2008. 296pp.en
dc.identifier.urihttp://hdl.handle.net/1773/3759
dc.description.abstractDissolved oxygen was measured at many stations in Glacier Bay. The purpose was to isolate the source of deep water renewal in the bay, and also to add to datasets of oceanographic observations. Glacier Bay is shallow silled, and light water spills over into the bay from Icy Strait, renewing the deep water.en
dc.language.isoen_USen
dc.publisherSchool of Oceanography, University of Washingtonen
dc.subjectHydrology--Alaska--Glacier Bayen
dc.subjectWater--dissolved oxygen--Alaska--Glacier Bay--observationsen
dc.titleDissolved oxygen within Glacier Bay: sources, deep basin values and comparison to other glacial fjordsen
dc.typeOtheren


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