Coastal upwelling supplies oxygen-depleted water to the Columbia River estuary.
Low dissolved oxygen (DO) is a common feature of many estuarine and shallow-water environments, and is often attributed to anthropogenic nutrient enrichment from terrestrial-fluvial pathways. However, recent events in the U.S. Pacific Northwest have highlighted that wind-forced upwelling can cause n...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Public Library of Science (PLoS)
2011-04-01
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| Series: | PLoS ONE |
| Online Access: | http://europepmc.org/articles/PMC3080374?pdf=render |