Synopsis (courtesy of NWS Chicago)
A very dynamic storm system impacted the area Wednesday night through Friday. This produced everything from some winter precipitation, to thunderstorms, dense fog, and even very strong winds across the area.
The storm system first developed across the plains on Wednesday. Then, as the system progressed eastward Wednesday night, it induced a strengthening wind field a couple thousand feet off the ground. This is typically referred to by meteorologists as a low level jet. This low level jet pumped warmer and very moist air northward across the Mississippi Valley to the Lower Great Lakes region Wednesday night. As this moisture reached northern Illinois, strong convergence occurred along the northern periphery of the strongest southerly wind field late Wednesday night into Thursday. This is highlighted in the figure below. Ultimately, this continual moisture convergence across Northern Illinois led to the development of moderate to heavy precipitation across the area during the predawn hours of Thursday morning.
Most areas just received periods of moderate to heavy rain from this initial surge of moisture late Wednesday night. However, areas across far northern Illinois, especially areas north of interstate 88, were cold enough for the precipitation to begin as a period of wet snow, sleet and freezing rain. This resulted in a quick 1 to 2 inches of heavy wet snow accumulation early Thursday morning across far northern Illinois from this initial band of precipitation. Elsewhere across the area, thunderstorms with periods of heavy rain were the rule into Thursday morning. Then, during the afternoon Thursday, a surface warm front begin lifting northward across the area. With a much warmer and very moist airmass associated with this warm front, the combination of the melting snow and rapidly increasing low level moisture resulted in the development of very dense fog area-wide. This fog produced near-zero visibilities for a few hours Thursday afternoon.
During the late afternoon and early evening on Thursday, a line of showers and thunderstorms moved across the region ahead of an approaching strong cold front. These storms did not reach severe limits across northern Illinois or northwestern Indiana. However, our neighbors to the south across central Illinois did experience some severe gusty thunderstorms, with even a couple of tornados reported across west central Illinois.
Finally, as the surface low moved into southern Wisconsin early Thursday evening, it pushed a strong cold front across the area. In the wake of this front the winds increased significantly out of the southwest. Winds gusted between 50 to 65 mph for a period Thursday evening following this frontal passage. The wind magnitudes were so strong due to the fact that the surface low continued to strengthen rapidly as it was moving northward across Wisconsin. This resulted in a very strong pressure gradient as surface high pressure set up across the southern United States.
Below is a loop of the satellite water vapor imagery (similar to the figure above). The blue colder colors show areas of enhanced moisture in the atmosphere, such as that from clouds and precipitation, while the warmer colors indicated drier areas in the atmosphere. This information is useful to meteorologists as we track storm systems across the country in real time. Also shown is the location and track of the surface low. The green arrows are the moisture transport vectors approximately 3,500 feet above the ground. This shows us that significant moisture was rapidly being transported northward from the Gulf of Mexico. A large influx of deep moisture is an important ingredient in heavy precipitation. Note that the loop starts late Wednesday night and runs through late Wednesday afternoon.
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