If you're planning a day at the beach in Chicago, beware: your body temperature might actually drop even though it's not directly over the water. According to Illinois state climatologist Trent Ford, this "cooler by the lake" phenomenon occurs when the land and air are warmer than the water.
As warm air rises off the city's hot concrete jungle, it cools down once it hits the relatively cool waters of Lake Michigan. This cooling effect can make a narrow strip of land around the lake as much as 80 degrees Fahrenheit cooler than the surrounding areas. The key is that this effect only occurs when there's a significant temperature difference between the water and the air.
Ford notes that this phenomenon typically happens in the spring and early summer, but its effects are more pronounced in late summer. However, by fall and winter, the process reverses: it takes longer for the lake to cool down than the surrounding land and air, resulting in a warmer-than-usual temperature near the water's edge.
If you're wondering just how close you need to be to Lake Michigan to experience this cooling effect, Ford estimates that it's about one mile west of Halsted Street. Even crossing over to the other side won't immediately make you warm up. However, by late summer, the lake's temperature increases enough that the "cooler by the lake" phenomenon disappears.
But there's another winter weather phenomenon related to Lake Michigan worth noting: lake-effect snow. When warm air from the south flows across a cold lake, it leads to significant snowfall in certain areas of the country. In Chicago, this usually happens when cold air moves from the west into the city and winds reverse direction over the lake.
However, for lake-effect snow to occur, several conditions need to be met: a low-pressure system must come from the south around Champaign or Kankakee, moist warm air needs to move across the cold lake, and strong winds are required to carry this moisture into Chicago. When these factors align, "lake-effect snow" can dump heavy snow on the city.
While it's rare for all these conditions to come together, they did in 2011 during a major blizzard known as Groundhog Day. This event highlighted just how unpredictable and dramatic Lake Michigan weather can be.
As warm air rises off the city's hot concrete jungle, it cools down once it hits the relatively cool waters of Lake Michigan. This cooling effect can make a narrow strip of land around the lake as much as 80 degrees Fahrenheit cooler than the surrounding areas. The key is that this effect only occurs when there's a significant temperature difference between the water and the air.
Ford notes that this phenomenon typically happens in the spring and early summer, but its effects are more pronounced in late summer. However, by fall and winter, the process reverses: it takes longer for the lake to cool down than the surrounding land and air, resulting in a warmer-than-usual temperature near the water's edge.
If you're wondering just how close you need to be to Lake Michigan to experience this cooling effect, Ford estimates that it's about one mile west of Halsted Street. Even crossing over to the other side won't immediately make you warm up. However, by late summer, the lake's temperature increases enough that the "cooler by the lake" phenomenon disappears.
But there's another winter weather phenomenon related to Lake Michigan worth noting: lake-effect snow. When warm air from the south flows across a cold lake, it leads to significant snowfall in certain areas of the country. In Chicago, this usually happens when cold air moves from the west into the city and winds reverse direction over the lake.
However, for lake-effect snow to occur, several conditions need to be met: a low-pressure system must come from the south around Champaign or Kankakee, moist warm air needs to move across the cold lake, and strong winds are required to carry this moisture into Chicago. When these factors align, "lake-effect snow" can dump heavy snow on the city.
While it's rare for all these conditions to come together, they did in 2011 during a major blizzard known as Groundhog Day. This event highlighted just how unpredictable and dramatic Lake Michigan weather can be.