@article {76596,
	title = {A method to identify estuarine water quality exceedances associated with ocean conditions},
	journal = {Environmental Monitoring and Assessment},
	volume = {187},
	year = {2015},
	note = {Major coastal upwelling events bring water that is low in oxygen and high in nutrients closer to the surface, at times killing marine animals.  Upwelled waters can and do enter estuaries.  Is there a way to distinguish poor water quality in estuaries that results from upwelling events from poor water quality derived from other causes?  The authors introduce an example of logistic regression models {\textquotedblleft}to predict the probability of exceedance of a water quality threshold{\textellipsis}{\textquotedblright}  Yaquina Bay is used as the example, and remaining issues are discussed.},
	month = {2015, Mar.},
	pages = {14 p.},
	keywords = {chlorophyll, climate, dissolved oxygen, mathematical modeling, salinity, upwelling, water quality, water temperature, Yaquina Bay},
	doi = {10.1007/s10661-015-4347-3},
	author = {Brown, Cheryl A. and Nelson, Walter G.}
}
@article {34441,
	title = {Historic and recent patterns of dissolved oxygen in the Yaquina Estuary (Oregon, USA): Importance of anthropogenic activities and oceanic conditions},
	journal = {Estuarine, Coastal and Shelf Science},
	volume = {92},
	number = {3},
	year = {2011},
	note = {Dissolved oxygen (DO) levels in estuaries can drop due to human activities.  They can also fall due to upwelling events offshore."This paper assesses whether there have been long-term changes in DO levels in the Yaquina Estuary, Oregon (USA) and the effect of ocean conditions on DO levels within that estuary. In addition, it compares  recent DO levels in the Yaquina Estuary to historical data from other estuaries in the region and the inner Oregon shelf to evaluate whether the hypoxia recently observed on the inner shelf has previously occurred." (from the Introduction)},
	month = {2011, May 1},
	pages = {p.446-455},
	keywords = {anoxia, dissolved oxygen, historical, upwelling, Yaquina Bay},
	doi = {10.1016/j.ecss.2011.01.018},
	author = {Brown, Cheryl A. and Power, James H.}
}
@inbook {51326,
	title = {Impacts of climate change on Oregon{\textquoteright}s coasts and estuaries},
	booktitle = {Oregon Climate Assessment Report},
	year = {2010},
	note = {This is Chapter 6 of the Oregon Climate Assessment Report. Predicts {\textquotedblleft}Increased winter{\textendash}early spring flow of coastal rivers and creeks and reduced flow during summer{\textquotedblright} for the Umpqua River (p.242)},
	pages = {p.211-268},
	publisher = {Oregon State University. College of Oceanic and Atmospheric Sciences. Oregon Climate Change Research Institute,},
	organization = {Oregon State University. College of Oceanic and Atmospheric Sciences. Oregon Climate Change Research Institute,},
	address = {Corvallis, Or.},
	keywords = {Alsea Bay, Alsea Spit, bacteria, Bayocean Spit, climate change, climate precipitation, coastal hazards, Columbia River estuary, Coos Bay, dissolved oxygen, El Nino, erosion, estuaries, geology, landslides, Nehalem Bay, Nehalem Spit, Neskowin (Or.), Netarts Bay, ocean acidification, Rockaway Beach, salinity, Salmon River Estuary, sea level, Siletz Bay, Tillamook Bay, water temperature, wave heights, Yachats River, Yaquina Bay},
	url = {https://digital.osl.state.or.us/islandora/object/osl\%3A637577},
	author = {Ruggiero, Peter and Brown, Cheryl A. and Komar, Paul D. and Allan, Jonathan C. and Reusser, Deborah A. and Lee II, Henry},
	editor = {Dello, Kathie and Mote, Philip W.}
}
