More Frequent Wind Events Hurting Lake Water Quality, U of G Study Finds

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A Lake Erie beach with cloudy water and white crests

A Lake Erie beach on a windy day (Pixabay)

Climate change is leading to poorer water quality in Lake Erie and may threaten nearby human and environmental health and the world’s largest commercial freshwater fishery, according to a new study led by University of Guelph researchers.

More frequent extreme wind events and currents are drawing up deep water whose low oxygen and high phosphorus may harm drinking water and fish in western Lake Erie, according to the paper published in Nature Scientific Reports.

Driven by global climate change, the same seasonal problem may play out in other large lakes with multiple basins, including other parts of the Great Lakes, said Dr. Joe Ackerman, professor in the Department of Integrative Biology.

The research was covered by The Associated Press with articles appearing in more than two dozen publications, including the Washington Post.

Dr. Josef Ackerman

Ackerman conducted the study with post-doc Dr. Aidin Jabbari and co-authors Dr. Leon Boegman, a professor of civil engineering at Queen’s University, and Dr. Yingming Zhao with the Ontario Ministry of Natural Resources and Forestry (OMNRF). The ministry monitors fish stocks for joint Canadian management with the United States through the Great Lakes Fishery Commission.

In shallow lakes and parts of freshwater bodies such as the western end of Lake Erie, winds normally keep water evenly mixed, providing consistent amounts of oxygen and nutrients.

Lake Erie is the shallowest of the Great Lakes. But it’s deep enough that in summer, water in its central and eastern basin divides into a warmer layer atop a colder layer. The dividing line between the two layers is called a thermocline.

Below the thermocline, respiration from organisms including microbial decomposition tends to use up oxygen during summer. Phosphorus from urbanization, industry and farms also ends up in the deeper water, which is ultimately low in oxygen and high in phosphorus.

A tripod of instruments, including turbidity sensors, temperature and oxygen meters, and fluorometers, ready for deployment into Lake Erie

Above the dividing line, the warmer water contains enough oxygen to support fish and is the location of drinking water intakes for nearby communities. The Lake Erie watershed is home to one out of three people living around the Great Lakes.

Ackerman said the problem arises with strong wind events, typically in August. Those winds cause powerful waves and currents that result in periodic upwelling of deeper, hypoxic (low oxygen) water, which can flow into the western basin. Under global warming, more strong winds and waves are occurring over Lake Erie.

“Wave power is increasing over time,” he said. “As weather warms, we will get larger waves and more powerful storms.”

His team looked at August records for the Great Lakes between 1980 and 2018. Over the period, they found increasing surface water temperature and wave power for that month were connected to atmospheric phenomena including El Nino.

“We found that extreme wind events have increased from one every other year to three a year from 1980 to 2018,” he said.

Dr. Aidin Jabbari (right) and PhD student Chris Farrow prepare the instrument tripod for deployment into Lake Erie

The currents caused by winds tilt the thermocline and pull up water with low oxygen and lots of phosphorus. In Lake Erie, that water from the deep central basin flows paradoxically into the shallower western basin, opposite to the normal flow direction.

The researchers found more hypoxic events in the western basin over the past 40 years, nearly half of them in the past decade. These changes can happen in a matter of hours, said Ackerman.

Hypoxia has been linked to periodic population declines in mayfly larvae, an important food for commercial fish such as walleye and yellow perch. These insects are a key indicator of water quality and overall ecological condition of the lake.

More phosphorus can also cause algae populations to bloom, including cyanobacteria that cause harmful algal blooms. That further reduces water quality, making it more difficult for fish to survive and potentially tainting drinking water. Upwelling of phosphorus would add to inputs of the element from the western end of the lake, including the Detroit and Maumee rivers.

Similar issues likely play out in other places with complex lake basins, including parts of the other Great Lakes affected by wind activity, said Ackerman.

He said the study might help resource managers in both Canada and the U.S. to connect upwelling – and the underlying wind-wave tandem driven by climate change – to changes in fish stocks in spot surveys.

“What causes hypoxia is important to lake ecosystems and to fisheries managers.”

The research was funded by the OMNRF and a Discovery grant from the Natural Sciences and Engineering Research Council of Canada.

Contact:

Dr. Josef Ackerman
ackerman@uoguelph.ca