The very windy autumn storm (click here for a detailed overview) which passed across the Great Lakes region late this past week produced some very impressive waves on Lake Michigan. The combination of winds occasionally gusting as high as 60 mph, and a long north-northwest fetch of up to 200 miles, resulted in waves building into the 20 to 25 foot range (trough to crest) on southern Lake Michigan late Thursday night and Friday. The NOAA south Lake Michigan buoy, around 50 miles east-southeast of Milwaukee, measured waves as high 23 feet at 4 am CDT Friday, The buoy sporadically lost wave height data during the period of maximum waves, possibly because of the extreme conditions. A tug captain at Burns Harbor Indiana estimated waves crashing over the break wall Friday morning to be in the 25 foot range! The graphic below is a rough estimation of the peak wave heights during the storm.
High resolution, true-color imagery from NASA's polar-orbiting AQUA-MODIS satellite, clearly shows the discoloration of the water in this image of Lake Michigan from Saturday afternoon. This is a 250 meter resolution image (each pixel is 250 meters square or 820 feet) taken from an orbit of approximately 438 miles above the earth's surface.
(Click the graphic to enlarge)
In addition to the discoloration of the lake due to the wave-churned sediment, the AQUA-MODIS image also clearly depicts stratocumulus clouds over and downwind of the lake. These clouds, which unfortunately become quite common across the lake in the cool season, form due to the advection of colder air over the still relatively mild lake waters. This results in an unstable thermodynamic profile, which leads to convective updrafts as the cold air traverses the warmer lake waters. Heat and moisture are transported upward from the surface of the lake by these updrafts, which develop into stratocumulus clouds as the moisture cools and condenses. If the cold air is sufficiently deep, these stratocumulus clouds may even produce lake-induced rain or snow showers. These clouds (or showers) typically align with the direction of the mean wind flow across the lake, and may extend well inland from the downwind shore. This is the "Lake Effect" of which residents of the Great Lakes region are so familiar with during the cold season. The following cross-sectional image depicts this process.
The sediment, and lake effect clouds from Saturday, can also be seen in 1 km resolution GOES weather satellite imagery. The following java loop from the visible channel of the GOES imager shows these processes in motion. Note that the clouds tend to follow the observed surface winds, which are indicated by the green barbs in the plotted observations. Warming temperatures aloft resulted in decreased lake-induced instability, and therefore shallower cloud depth and gradual dissipation of clouds during the course of the afternoon.
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Ratzer/Shea - 01 October 2011