Scientists from the University of Rhode Island and colleagues in the U.S. and Canada have found the water level in the Great Lake system is highly sensitive to climate changes.
The water level in the Great Lakes has varied by only about two meters during the last century, helping them to play a vital role in the region’s shipping, fishing, recreation and power generation industries.
This new evidence was published
last month in the journal Eos,
and indicates that the water level in the lake system is highly sensitive to climate changes.
“In the distant past, there were great fluctuations in the water level of the Great Lakes, but it was thought to have been related entirely to the advance and retreat of the glaciers,” said URI geological oceanographer John King, who led the study with URI visiting scientist Michael Lewis, emeritus scientist with the Geological Survey of Canada.
“But the last time lake levels fell dramatically – down to 20 meters below the basin overflow outlets – it was due to dry climate conditions.”
That event, which occurred between 7900 and 7500 years ago in the early Holocene period, caused the lakes to become disconnected as their overflow rivers, including the Niagara River, ran dry.
“People used to say that the oceans are so big, we can dump whatever we want in them and nothing will happen,” said King.
“They thought of the Great Lakes in the same way, that the system is too large to be sensitive to climate variations. But now we know that to be untrue. We’ve demonstrated that at least once in the last 10,000 years, climate drove the lake levels down pretty substantially.”
Researchers have assumed the Great Lakes had been “hydrologically open” and connected since their formation 16,000 years ago during the retreat of the last ice sheet, but recent evidence has found this to be false. Ancient shorelines, submerged beaches, and tree stumps on the floor of some lakes indicate that the water line had been as much as 20 meters below the present lake level.
“We had a multi-proxy approach to this study, and through many lines of evidence we identified this as a dry interval with a climactic cause as opposed to a glacial-related cause,” King said.
The climate and water levels in the Great Lakes region are determined by the interplay of three air masses: dry, cold Arctic air from the North, dry warm Pacific air from the West, and warm, moist tropical air from the Gulf of Mexico.
The researchers found during the period when lake levels receded significantly, the dry air from the Arctic and Pacific was dominant. Later, when precipitation from the tropical air mass became more frequent, the Great Lakes began to flow from one to another as they do today.
“The climate interval that occurred back then is different from what we’re going through now,” King said
. “It would take a pretty big change to close the basins again. But the sorts of temperatures and precipitation amounts that happened then are within the range of what is predicted for 2100. In the worst-case scenarios, a lot of things become possible.
“The range of lake-level changes that are likely to happen in the next 100 years is probably larger than the range of levels observed during the last century,” he added.