National Weather Service United States Department of Commerce

 

Radar Loop

NWS Chicago Doppler Radar loop and airport observations from 1 a.m. through 5 a.m. on July 16.  Note light reflectivity moving southward across the Chicago metro area. It's passage correlated to:

1.) a sharp drop in air pressure likely due to a wake low,

2.) strong wind gusts correlating with the pressure change,

3.) then shortly after, a rapid jump in temperature and

4.) a drop in moisture.  

The last two in this list are particularly interesting.

This light reflectivity and associated rapid weather change originated from storms that had quickly dissipated over far southeast Wisconsin. Notice how storms quickly collapse across McHenry and Kane Counties too which may have also had an effect.

 

...Maximum Wind Gusts...

Location                     Speed     Time/Date     
---------------------------------------------------- 
Chicago Midway               40 MPH    0331 AM 07/16  
Rockford Airport             39 MPH    0322 AM 07/16
Chicago O'Hare               37 MPH    0254 AM 07/16 
Kankakee Airport             37 MPH    0533 AM 07/16 
Chicago Harrison-Dever Crib  36 MPH    0300 AM 07/16      
Dupage Airport               32 MPH    0402 AM 07/16          
Lewis Airport, Romeoville    31 MPH    0455 AM 07/16

 

ORD Observations

 

 

ORD Trace

Chicago O'Hare International Airport observations, with the box indicating the observed sharp warming and drying.  The temperature warmed from 72° to 79° between 3:05 a.m. and 3:30 a.m.

 

MDW Observations

 

 

MDW Trace

Chicago Midway International Airport observations, with the box indicating the observed warming and drying.  The temperature warmed from 73° to 81° between 3:45 a.m. and 3:55 a.m.

 

Heat Burst Info
Heat burst infographic courtesy of NWS Sioux Falls, SD.  A heat burst, or at least a phenomenon with similar traits, is suspected to have occurred in northeast Illinois during the early morning of July 16 . Typically a true heat burst happens over a smaller area and closer to where the storms collapsed than what was observed. Also, they are most commonly found in the Plains states, though still not common. They are exceptionally rare in northern Illinois.