![\"GOES-16](\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/03\/210320_goes16_visible_infrared_FL_anim.gif\")
<\/a>GOES-16 \u201cRed\u201d Visible (0.64 \u00b5m)<\/em> and “Clean” Infrared Window (10.35 \u00b5m)<\/em> images [click to play animation | MP4<\/strong><\/a>]<\/p><\/div>GOES-16 (GOES-East)<\/em> \u201cRed\u201d Visible (0.64 \u00b5m<\/strong><\/a>) and \u00a0\u201cClean\u201d Infrared Window (10.35 \u00b5m<\/strong><\/a>) images\u00a0(above) <\/strong><\/em>displayed the development of a small nor’easter-type low off the coast of northeastern Florida on 20 March 2021<\/strong><\/a>. Onshore winds kept low clouds\/fog and light precipitation along the coast for much of the day — and surface wind gusts were as high as 41 knots at Buoy 41009<\/strong><\/a> just east of Cape Canaveral.<\/p>\n GOES-16 Visible and Infrared images on the following day (below)<\/strong> <\/em>showed that the surface low had remained quasi-stationary as it transitioned to its occluded phase. Thunderstorm development persisted farther offshore over the warm waters of the Gulf Stream — a few overshooting tops exhibited infrared brightness temperatures of -60\u00baC and colder.<\/p>\n GOES-16 \u201cRed\u201d Visible (0.64 \u00b5m)<\/em> and “Clean” Infrared Window (10.35 \u00b5m)<\/em> images [click to play animation | MP4<\/strong><\/a>]<\/p><\/div>The prolonged period of strong winds associated with this low pressure feature induced an upwelling of cooler water, as shown in a plot of Water Temperature at Buoy 41009 (below)<\/strong><\/em>.<\/p>\n<\/a>