{"id":44698,"date":"2022-02-18T22:49:54","date_gmt":"2022-02-18T22:49:54","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=44698"},"modified":"2022-02-25T15:38:05","modified_gmt":"2022-02-25T15:38:05","slug":"snow-squall-warnings-over-duluth-minnesota-and-northwestern-wisconsin","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/44698","title":{"rendered":"Snow Squall Warnings over Duluth Minnesota and northwestern Wisconsin"},"content":{"rendered":"\n<figure class=\"wp-block-image size-large\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/02\/G16DCPD-20220218_1731_to_2046anim.gif\"><img loading=\"lazy\" decoding=\"async\" width=\"1302\" height=\"909\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/02\/G16DCPD-20220218_1731_to_2046anim.gif\" alt=\"\" class=\"wp-image-44710\" \/><\/a><figcaption>GOES-16 Day Cloud Phase Distinction 1731 &#8211; 2046 UTC on 18 February 2022 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<p>The animation above, of the Day Cloud Phase Distinction RGB, shows bands of snow showers\/squalls rotating cyclonically through northern Minnesota and northwestern Wisconsin, to the south of a strong cyclone over northern Minnesota and northwestern Ontario (<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/02\/nasfc021822_221002.gif\">link to map<\/a> from 1800 UTC on 18 February).  The tops of these clouds are fairly low &#8212; in the RGB they have a periwinkle color in contrast to the orange\/red color of the higher cirrus to the south.  The RGB also allows for good contrast between the clouds and the clear snow-covered grounds (with greenish tones) to the west.<\/p>\n\n\n\n<p>A potency of the upper air system supporting the surface cyclone is highlighted in the Ozone Anomaly fields from gridded NUCAPS data, shown below.  Anomalies of 120-140 dobson Units are present.<\/p>\n\n\n\n<figure class=\"wp-block-image size-full\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/02\/NUCAPSOzoneAnomaly-20220218_1730_1930toggle.gif\"><img loading=\"lazy\" decoding=\"async\" width=\"877\" height=\"490\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/02\/NUCAPSOzoneAnomaly-20220218_1730_1930toggle.gif\" alt=\"\" class=\"wp-image-44714\" \/><\/a><figcaption>NUCAPS estimates of Ozone Anomaly at 1730 and 1930 UTC on 18 February 2022 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<p>The <a href=\"https:\/\/weather.gov\/dlh\/\">National Weather Service in Duluth MN<\/a> issued a series of Snow Squall Warnings; the first one, valid until 1945 UTC, is shown below (taken from <a href=\"https:\/\/twitter.com\/NWSduluth\/status\/1494754426002690048\">this tweet<\/a>); sequential tweeted Warnings are <a href=\"https:\/\/twitter.com\/NWSduluth\/status\/1494760320090271744\">here<\/a> (valid until 2015 UTC), <a href=\"https:\/\/twitter.com\/NWSduluth\/status\/1494771715817177088\">here<\/a> (valid until 2100 UTC), <a href=\"https:\/\/twitter.com\/NWSduluth\/status\/1494782940189839360\">here<\/a> (valid until 2145 UTC) and <a href=\"https:\/\/twitter.com\/NWSduluth\/status\/1494787048271609857\">here<\/a> (valid until 2215 UTC).  (Note, WFO ARX &#8212; in Lacrosse, WI, is issuing Snow Squall warnings for this system as well!)<\/p>\n\n\n\n<figure class=\"wp-block-image size-full\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/02\/SnowSquallWarning.png\"><img loading=\"lazy\" decoding=\"async\" width=\"979\" height=\"742\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/02\/SnowSquallWarning.png\" alt=\"\" class=\"wp-image-44699\" srcset=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/02\/SnowSquallWarning.png 979w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/02\/SnowSquallWarning-300x227.png 300w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/02\/SnowSquallWarning-768x582.png 768w\" sizes=\"auto, (max-width: 979px) 100vw, 979px\" \/><\/a><figcaption>NWS Duluth Graphic of snow squall warning for 18 February 2022, for the time period ending 1945 UTC (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<p>Three radars for this event are shown below: 1907, 1937 and 2007 UTC.  <\/p>\n\n\n\n<figure class=\"wp-block-image size-full\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/02\/Radar1907_1937_2007step.gif\"><img loading=\"lazy\" decoding=\"async\" width=\"990\" height=\"870\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/02\/Radar1907_1937_2007step.gif\" alt=\"\" class=\"wp-image-44700\" \/><\/a><figcaption>Radar Reflectivity at 1907, 1937 and 2007 UTC on 18 February 2022 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<p>VIIRS imagery (available from the CIMSS LDM feed) over the Duluth Area afforded a high-resolution view of this event.  The toggles below show True and False Color imagery at 1838 UTC (from Suomi NPP) and at 1929 UTC (from NOAA-20)  At 1838 UTC, the clouds producing the snow &#8212; between Moose Lake and Floodwood &#8212; do not stand out.  They are much more noticeable in the 1929 UTC image, southeast of Duluth and northwest of Solon Springs.<\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/02\/VIIRSTrueFalseColor-20220218_1838toggle.gif\"><img loading=\"lazy\" decoding=\"async\" width=\"1302\" height=\"909\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/02\/VIIRSTrueFalseColor-20220218_1838toggle.gif\" alt=\"\" class=\"wp-image-44722\" \/><\/a><figcaption>True and False Color imagery, Suomi-NPP VIIRS, 1838 UTC on 18 February 2022 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<figure class=\"wp-block-image size-large\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/02\/VIIRSTrueFalseColor-20220218_1929toggle.gif\"><img loading=\"lazy\" decoding=\"async\" width=\"1302\" height=\"909\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/02\/VIIRSTrueFalseColor-20220218_1929toggle.gif\" alt=\"\" class=\"wp-image-44705\" \/><\/a><figcaption>True and False Color imagery, NOAA-20 VIIRS, 1929 UTC on 18 February 2022 (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<hr class=\"wp-block-separator\" \/>\n\n\n\n<p>What was the effect on visibility?  That is shown in the animation below with a 10-minute time step.  Note how Duluth goes from southwesterly winds with light snow and 5- to 10- mile visibility to strong northwest winds (gusts to 45 knots) and reduced visibilities as the squall moves through.<\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/02\/G16DCPDObs-20220218_1731_to_204110min.gif\"><img loading=\"lazy\" decoding=\"async\" width=\"1302\" height=\"909\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/02\/G16DCPDObs-20220218_1731_to_204110min.gif\" alt=\"\" class=\"wp-image-44711\" \/><\/a><figcaption>GOES-16 Day Cloud Phase Distinction 1731 &#8211; 2041 UTC on 18 February 2022 along with surface observations (Click to enlarge)<\/figcaption><\/figure>\n\n\n\n<hr class=\"wp-block-separator\" \/>\n\n\n\n<p>As this front moved through southern Wisconsin, it generated lightning, as shown in the animation below (from <a href=\"https:\/\/www.star.nesdis.noaa.gov\/GOES\/sector_band.php?sat=G16&amp;sector=cgl&amp;band=EXTENT3&amp;length=36&amp;dim=1\">this website<\/a>).<\/p>\n\n\n\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"600\" height=\"600\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/02\/G16_sector_cgl_EXTENT3_36fr_20220218-2032.gif\" alt=\"\" class=\"wp-image-44740\" \/><figcaption>GLM Flash Extent Density overlain on top of nighttime GeoColor, 2236 18 February &#8211; 0126 UTC 19 February 2022 (Click to enlarge)<\/figcaption><\/figure>\n","protected":false},"excerpt":{"rendered":"<p>The animation above, of the Day Cloud Phase Distinction RGB, shows bands of snow showers\/squalls rotating cyclonically through northern Minnesota and northwestern Wisconsin, to the south of a strong cyclone over northern Minnesota and northwestern Ontario (link to map from 1800 UTC on 18 February). The tops of these clouds are fairly low &#8212; in [&hellip;]<\/p>\n","protected":false},"author":19,"featured_media":44711,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[10,76,74,78,83,49,48],"tags":[],"class_list":["post-44698","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-general-interpretation","category-glm","category-goes-16","category-noaa-20","category-nucaps","category-suomi_npp","category-viirs"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/44698","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/users\/19"}],"replies":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/comments?post=44698"}],"version-history":[{"count":21,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/44698\/revisions"}],"predecessor-version":[{"id":44803,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/44698\/revisions\/44803"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/44711"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=44698"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=44698"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=44698"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}