Daytime lake breezes pull cool air inland then reverse after sunset
Land heats faster than lake water by day, so cooler air slides ashore as a lake breeze while warmer air rises inland. After sunset the land cools quicker and a land breeze often drifts toward the water.
Coastal towns around big lakes feel the pulse as a daily wind shift that can break heat or bring lake-cooled evenings. Sailors and sailplanes ride the circulation.
A lake is a thermal engine for the air above it. Lake and land breezes turn a quiet shoreline into a clockwork microclimate.
Comments
0 comments