![](\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/11\/211122_goes16_visible_nearInfraredSnowIce_WI_IL_hole_punch_clouds_anim.gif\")
<\/a>GOES-16 \u201cRed\u201d Visible (0.64 \u00b5m) and Near-Infrared “Snow\/Ice” (1.61 \u00b5m) images [click to play animated GIF | MP4<\/strong><\/a>]<\/p><\/div>GOES-16 (GOES-East)<\/em> \u201cRed\u201d Visible (0.64 \u00b5m<\/strong><\/a>) and Near-Infrared “Snow\/Ice” (1.61 \u00b5m<\/strong><\/a>) images (above)<\/strong><\/em> revealed the formation of several “hole punch” features across southeastern Wisconsin, northeastern Illinois and Lake Michigan on 22 November 2021<\/strong><\/a> . These cloud features were caused by aircraft that were either ascending or descending through a relatively thin layer of clouds composed of supercooled water droplets \u2014 cooling from wake turbulence (reference<\/strong><\/a>) and\/or particles from the jet engine exhaust acted as ice condensation nuclei, causing the small supercooled water droplets to turn into larger ice crystals (many of which then fall from the cloud layer, creating \u201cfallstreak holes<\/strong><\/a>\u201c). The ice crystal clouds appear as darker shades of gray on the 1.61 \u00b5m Snow\/Ice images.<\/p>\n The GOES-16 Cloud Top Temperature<\/strong><\/a> derived product (below)<\/strong><\/em> showed that values were generally in the -30 to -35\u00baC range.<\/p>\n GOES-16 Cloud Top Temperature product [click to play animated GIF | MP4<\/strong><\/a>]<\/p><\/div>A toggle between 250-meter resolution Terra MODIS True Color and False Color RGB images from the MODIS Today<\/a><\/strong> site (below)<\/strong><\/em> provided a more detailed view of the numerous hole punch features at 1730 UTC, including a better depiction of the glaciated fallstreak clouds (shades of cyan)<\/em> within the middle of each hole punch.<\/p>\n<\/a>