Dissolved oxygen within Glacier Bay: sources, deep basin values and comparison to other glacial fjords
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Authors
Helman, Dan
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School of Oceanography, University of Washington
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.
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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.