The water managed to get this cold through upwelling, which
occurs when cold waters towards the bottom of a body of water rises towards the
surface. WOOD-TV meteorologist Bill Steffen described what caused the upwelling
event:
We had a strong north wind behind a cold front and that pushed the surface water toward the middle of the lake, allowing much colder water from 100 feet below to rise to the surface.
The cold water's effect on the weather will remain
localized, with cooler temperatures along the coast as well as persistent fog
over coastal waters.
As seen by the satellite imagery at the top of this post,
the rapidly-chilled water created a thick layer of fog on Lake Michigan where
temperatures dropped the most. The cold water cooled the air above it through
conduction, dropping the air temperature to its dew point and condensing its
water vapor.
The average temperature for Lake Michigan at the end of July
is around 68°F, and the average temperature for Lake Superior sits around 60°F.
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