4.3 Article

Episodic nearshore-offshore exchanges of hypoxic waters along the north shore of Lake Erie

Journal

JOURNAL OF GREAT LAKES RESEARCH
Volume 47, Issue 2, Pages 419-436

Publisher

ELSEVIER SCI LTD
DOI: 10.1016/j.jglr.2021.01.014

Keywords

Lake Erie; Hypoxia; Nearshore-offshore exchanges; Hypoxic duration; Coastal upwelling events

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The study examines the nearshore-offshore exchange of hypoxic waters in northern Lake Erie during episodic coastal upwelling events, finding that wind-induced upwelling events play a dominant role in transporting low-oxygen waters to offshore regions. These events lead to temporal and spatial variations in oxygen levels and pH in nearshore waters, impacting oxygen levels near the lake bed.
We investigate the nearshore-offshore exchange of hypoxic waters during episodic coastal upwelling events in the nearshore waters of northern Lake Erie using intensive field observations and a validated hydrodynamic and water quality model. We observe wind-induced coastal upwelling events to be the dominant nearshore physical process in the lake which are energized every 5-10 days. When the winds were predominantly blowing from the west or south-west, epilimnetic waters were transported to the offshore bringing in hypolimnetic waters with low temperature (8-10 degrees C), dissolved oxygen (DO: 06 mg L-1) and pH (6-7) to the nearshore zones. During these events, vertical diffusivity coefficients decreased from 10(-2) m(2) s(-1) to values as low as similar to 10(-7) m(2) s(-1). In late summer, the coastal upwelling events in the nearshore waters lower the near bottom DO to hypoxic levels (DO < 2 mg L-1). Lakewide observations of DO and pH show that they are positively and linearly correlated while in the nearshore DO and pH experience spatial and temporal variability where upwelling events were developed, which were further assessed using a three-dimensional model. The model accuracy to reproduce offshore hypoxia was first assessed on a lake-wide basis using a coarse resolution model for a five-year period (2008-2012) and in nearshore waters using a higher resolution model for 2013. We use the model results to delineate the near bottom areas experiencing hypoxia at time scales longer than 48 h. (C) 2021 The Author(s). Published by Elsevier B.V. on behalf of International Association for Great Lakes Research.

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