Lake Michigan’s hidden waters spread rapidly

By Sohail Khan 9 September 2026, 7:39 pm

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Business News›News›International›Global Trends›Lake Michigan looks calm from shore, but a 2013 11 kg of red dye experiment revealed its hidden waters can spread far faster than scientists expected

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Lake Michigan looks calm from shore, but a 2013 11 kg of red dye experiment revealed its hidden waters can spread far faster than scientists expected
Synopsis

A 2013 dye experiment in Lake Michigan revealed that water in the lake’s open interior can spread surprisingly quickly. Researchers traced a fluorescent dye plume for hours and found that near-surface shear linked to Poincaré waves helped drive unexpectedly rapid dispersion. Researchers observed the dye's dispersion rate increase from approximately 1.5 to 4.2 square metres per second over about 21 hours.

Stretching for more than 500 kilometres and bordered by Wisconsin, Michigan, Illinois and Indiana, Lake Michigan is the only one of the five Great Lakes located entirely within the United States.

From the shoreline, it can look remarkably peaceful. Gentle ripples move across the surface, often giving little indication of the powerful movements taking place beneath the water.

But a remarkable 2013 experiment revealed that the lake's seemingly quiet interior can be surprisingly dynamic.

Scientists released fluorescent dye into Lake Michigan

Researchers from Purdue University, working with NOAA's Great Lakes Environmental Research Laboratory, wanted to answer a difficult question: How quickly does a patch of water spread once it moves into the open lake, far from the shoreline?

To find out, the team traveled aboard the research vessel Blue Heron and released 11 kilograms of Rhodamine WT, a fluorescent tracer that makes water detectable as a pink-red plume.

The dye was carefully mixed with ethanol and lake water so its density matched the surrounding surface layer. Scientists then pumped it through a floating diffuser, allowing it to disperse evenly instead of sinking or forming one concentrated mass.

Within hours, the dye had transformed from a relatively compact cloud into a much larger, irregular patch.

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The pink plume revealed how fast the water was moving

Researchers used fluorometers to track the dye as it spread through the lake. For roughly 21 hours, they watched the plume stretch, fold and move with the currents.

An AI-generated image showing researchers releasing fluorescent Rhodamine WT dye into Lake Michigan to track how water spreads and mixes offshore. Credits – Google Gemini

The dye was carefully mixed with ethanol and lake water so its density matched the surrounding surface layer (AI generated)

What they were trying to calculate was the dispersion coefficient, a measurement that describes how rapidly a substance spreads through water.

Scientists had generally expected dispersion to be slower in the deep, open portions of a lake because the water there is far from the shoreline and lake bottom. Near coastal areas, friction and wave activity can strongly disturb water movement.

The results from Lake Michigan told a different story.

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The dispersion rate climbed dramatically

During the experiment, the researchers observed the dye's dispersion rate increase from approximately 1.5 to 4.2 square metres per second over about 21 hours.

That was unexpectedly rapid for a dye patch released so far from shore.

The researchers concluded that near-surface shear associated with near-inertial Poincaré waves helped explain the unusually high dispersion rates.

These waves are internal movements within a stratified lake. During summer, Lake Michigan develops distinct layers, with warmer water near the surface and colder water underneath.

The resulting movements can create differences in velocity between layers. That vertical shear stretches the dye plume, helping it spread across a much larger area.

A second experiment showed the lake can behave differently

The scientists also used floating drifters during a longer experiment lasting 24 days.

Initially, the drifters showed slower and more gradual movement under relatively calm conditions. But when stronger winds arrived, their dispersal became faster and more irregular.

Together, the observations showed that open-water mixing in Lake Michigan is not governed by one simple process. Conditions such as stratification, waves and wind can dramatically influence how material moves across the lake.

Why Lake Michigan's hidden currents matter

The findings are important far beyond understanding an unusual movement of water.

Knowing how quickly substances disperse in Lake Michigan can help scientists model what could happen after an accidental spill. It can also improve predictions about how agricultural nutrients travel through the lake and how heat is redistributed as climate conditions change.

Earlier research had shown that mixing can be strong near shorelines because of waves and bottom friction. The 2013 dye experiment demonstrated that the vast open interior of the lake can also experience surprisingly vigorous mixing, even without a nearby shoreline.

For a lake that can appear almost motionless from the beach, the experiment offered a striking reminder: beneath the calm surface of Lake Michigan, the water is constantly moving, stretching and mixing in ways the human eye cannot see.

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Lake MichiganLake Michigan experimentGreat LakesRhodamine WTfluorescent dyewater dispersionPoincaré waveslake currentswater mixingPurdue University

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