![\"GOES-17](\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2020\/12\/201221_goes17_shortwaveInfrared_infraredWindow_Kilauea_eruption_HI_anim.gif\")
<\/a>GOES-17 Shortwave Infrared (3.9 \u00b5m)<\/em> and “Clean” Infrared Window (10.35 \u00b5m)<\/em> images [click to play animation | MP4<\/strong><\/a>]<\/p><\/div>GOES-17 (GOES-West)<\/em> Shortwave Infrared (3.9 \u00b5m<\/strong><\/a>) and “Clean” Infrared Window (10.35 \u00b5m<\/strong><\/a>) images (above)<\/strong> <\/em>displayed the thermal anomaly (cluster of hot pixels) and brief volcanic cloud resulting from an eruption of the Kilauea volcano on the Big Island of Hawai’i on 21 December 2020. The coldest cloud-top 10.35 \u00b5m infrared brightness temperature was -34.6\u00baC at 0840 UTC — which roughly corresponded to the 300 hPa or 9.6 km altitude according to 12 UTC rawinsonde data from nearby Hilo (plot<\/strong><\/a> | text<\/strong><\/a>). However, this volcanic cloud quickly dissipated in the very dry air aloft.<\/p>\n GOES-17 Near-infrared (1.61 \u00b5m<\/strong><\/a> and 2.24 \u00b5m<\/strong><\/a>) and Shortwave Infrared images (below)<\/strong><\/em> showed the variation in thermal signatures during the hours leading up to sunrise. The signature in Near-Infrared imagery was occasionally attenuated by the passage of trade wind cumulus clouds over the eruption site.<\/p>\n GOES-17 Near-infrared (1.61 \u00b5m and 2.24 \u00b5m)<\/em> and Shortwave Infrared (3.9 \u00b5m)<\/em> images [click to play animation | MP4<\/strong><\/a>]<\/p><\/div>A comparison of Suomi NPP VIIRS Near-infrared (1.61 \u00b5m and 2.25 \u00b5m), Shortwave Infrared (3.75 \u00b5m) and Day\/Night Band (0.7 \u00b5m) images (below)<\/strong><\/em> provided a high spatial resolution view of the thermal and emitted light signatures of the ongoing eruption at 1221 UTC.<\/p>\n Suomi NPP VIIRS Near-infrared (1.61 \u00b5m and 2.25 \u00b5m),<\/em> Shortwave Infrared (3.75 \u00b5m)<\/em> and Day\/Night Band (0.7<\/em> \u00b5m)<\/em> images (credit: William Straka, CIMSS) [click to enlarge]<\/p><\/div>A larger-scale view of GOES-17 Shortwave Infrared, SO2 RGB<\/strong><\/a> and Ash RGB<\/strong><\/a> images (below)<\/strong> <\/em>showed the southward transport of a mid\/high-altitude plume of SO2 (lighter shades of yellow to cyan)<\/em> from the initial eruption, followed by the southwestward transport of a more persistent low-altitude plume of SO2 as the eruption continued during the day. No signature of volcanic ash was indicated (either qualitatively on the Ash RGB images, or on retrieved ash products<\/strong><\/a> from this site<\/strong><\/a>). At times the thermal anomaly of the eruption site exhibited 3.9 \u00b5m infrared brightness temperatures as hot as 105\u00baC.<\/p>\n GOES-17 Shortwave Infrared (3.9 \u00b5m),<\/em> SO2 RGB and Ash RGB images [click to play animation | MP4<\/strong><\/a>]<\/p><\/div>GOES-17 True Color RGB images created using Geo2Grid<\/strong><\/a> (below)<\/strong> <\/em>displayed the volcanic fog (or “vog”) plume that moved southwestward during the day — a portion of which became entrained into the circulation of a lee-side cyclonic gyre southwest of the Big Island.<\/p>\n<\/a><\/a><\/a>