In 2013, scientists released 11 kg of red dye into Lake Michigan to measure offshore mixing; the study recorded dispersion rising from 1.5 to 4.2 m²/s over about 21 hours

In a groundbreaking study, researchers uncovered concealed currents stirring the waters of Lake Michigan away from its shores. A dye experiment showcased astonishing dispersion speeds, illustrating that these internal waves, invisible from the surface, significantly enhance water mixing. This revelation questions earlier beliefs regarding the movement of open lake water and is crucial for improving spill predictions and nutrient flow understanding.
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