Dissolved oxygen within Glacier Bay: sources, deep basin values and comparison to other glacial fjords

ResearchWorks/Manakin Repository

Search ResearchWorks


Advanced Search

Browse

My Account

Statistics

Related Information

Dissolved oxygen within Glacier Bay: sources, deep basin values and comparison to other glacial fjords

Show simple item record

dc.contributor.author Helman, Dan
dc.date.accessioned 2008-07-23T18:03:01Z
dc.date.available 2008-07-23T18:03:01Z
dc.date.issued 2008-06-19
dc.identifier.citation Keil 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.uri http://hdl.handle.net/1773/3759
dc.description.abstract Dissolved 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.iso en_US en
dc.publisher School of Oceanography, University of Washington en
dc.subject Hydrology--Alaska--Glacier Bay en
dc.subject Water--dissolved oxygen--Alaska--Glacier Bay--observations en
dc.title Dissolved oxygen within Glacier Bay: sources, deep basin values and comparison to other glacial fjords en
dc.type Other en


Files in this item

Files Size Format View
dhelman.pdf 1.410Mb PDF View/Open

This item appears in the following Collection(s)

Show simple item record