{"id":39783,"date":"2021-02-02T19:59:38","date_gmt":"2021-02-02T19:59:38","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=39783"},"modified":"2021-02-05T15:55:34","modified_gmt":"2021-02-05T15:55:34","slug":"northeast-us-winter-storm-3","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/39783","title":{"rendered":"Northeast US winter storm"},"content":{"rendered":"<p><div style=\"width: 652px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/02\/210201_goes16_waterVapor_precipType_Northeast_US_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/02\/G16_WV_WX1_NEUS_WINTER_STORM_01FEB2021_B9_2021032_180611_GOES-16_0001PANEL_FRAME0000110.GIF\" alt=\"GOES-16 Mid-level Water Vapor (6.9 \u00b5m) images, with plots of hourly surface weather type [click to play animation | MP4]\" width=\"642\" height=\"602\" \/><\/a><p class=\"wp-caption-text\">GOES-16 Mid-level Water Vapor <em>(6.9 \u00b5m)<\/em> images, with hourly surface weather type plotted in red [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/02\/210201_goes16_waterVapor_precipType_Northeast_US_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>GOES-16 <em>(GOES-East)<\/em> Mid-level Water Vapor (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band09.pdf\"><strong>6.9 \u00b5m<\/strong><\/a>) images with plots of hourly surface weather type <em><strong>(above) <\/strong><\/em>showed the formation of a well-defined cold conveyor belt that moved westward across parts of the Northeast US during the <a href=\"https:\/\/www.wpc.ncep.noaa.gov\/dailywxmap\/index_20210201.html\"><strong>01 February<\/strong><\/a> &#8211; <a href=\"https:\/\/www.wpc.ncep.noaa.gov\/dailywxmap\/index_20210202.html\"><strong>02 February 2021<\/strong><\/a> period. This moist airstream helped to enhance snowfall rates, with 2-4 inches per hour occurring at some locations. <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/02\/210202_snowfall_pns.text\"><strong>Storm total snowfall accumulations<\/strong><\/a> were as high as 36.1&#8243; in Pennsylvania, 35.5&#8243; in New Jersey, 25.6&#8243; in New York, 24.0&#8243; in Massachusetts, and 19.0&#8243; in Connecticut.<\/p>\n<p>Another feature that played an important role in enhancing\/prolonging heavy snowfall rates was a <a href=\"http:\/\/rammb.cira.colostate.edu\/training\/visit\/training_sessions\/trowal_identification\/\"><strong>TROWAL<\/strong><\/a> &#8212; appearing as a tongue of higher Equivalent Potential Temperature within the 850-700 hPa layer, just north of the surface occluded front &#8212; moving inland and feeding moisture into the southern edge of the cold conveyor belt seen on GOES-16 Water Vapor imagery <em><strong>(below)<\/strong><\/em>.<\/p>\n<div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/02\/210201_goes16_waterVapor_trowal_Northeast_US_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/02\/neus_trowal-20210201_180111.png\" alt=\"GOES-16 Mid-level Water Vapor (6.9 \u00b5m) images, with contours of 850-700 hPa layer Equivalent Potential Temperature (red) and Surface Fronts (purple) [click to play animation | MP4]\" width=\"641\" height=\"299\" \/><\/a><p class=\"wp-caption-text\">GOES-16 Mid-level Water Vapor <em>(6.9 \u00b5m)<\/em> images, with contours of 850-700 hPa layer Equivalent Potential Temperature <em>(red)<\/em> and Surface Frontal Analysis <em>(purple)<\/em> [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/02\/210201_goes16_waterVapor_trowal_Northeast_US_anim.mp4\"><strong>MP4<\/strong><\/a>]<span style=\"font-size: 16px;\">\u00a0<\/span><\/p><\/div>\n<p><center><\/p>\n<blockquote class=\"twitter-tweet\">\n<p dir=\"ltr\" lang=\"en\">Updated January 30-February 2 snowfall reports based on reports received as of 6 pm Tuesday. Here are the latest highest totals in each state (1 of 2).<br \/>\nPA &#8211; Nazareth 36.1&#8243;<br \/>\nNJ &#8211; Mount Arlington 35.5&#8243;<br \/>\nNY &#8211; Fishkill\/Saugerties 25.6&#8243;<br \/>\nMA &#8211; Lowell 24&#8243;<br \/>\nWV &#8211; Terra Alta 22.1&#8243; <a href=\"https:\/\/t.co\/unxodO5ccS\">pic.twitter.com\/unxodO5ccS<\/a><\/p>\n<p>\u2014 NWS Eastern Region (@NWSEastern) <a href=\"https:\/\/twitter.com\/NWSEastern\/status\/1356741384464719872?ref_src=twsrc%5Etfw\">February 2, 2021<\/a><\/p><\/blockquote>\n<p><script async src=\"https:\/\/platform.twitter.com\/widgets.js\" charset=\"utf-8\"><\/script><\/p>\n<p><\/center><br \/>\n1-minute\u00a0<a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/23225\"><strong>Mesoscale Domain Sector<\/strong><\/a>\u00a0GOES-16 \u00a0\u201cRed\u201d Visible (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band02.pdf\"><strong>0.64 \u00b5m<\/strong><\/a>) images with 5-minute plots of <a href=\"http:\/\/rammb.cira.colostate.edu\/training\/visit\/training_sessions\/goes_r_derived_motion_vectors\/\"><strong>Derived Motion Winds<\/strong><\/a> <em><strong>(below)<\/strong><\/em> revealed a mesoscale circulation just south-southwest of the analyzed location of the surface low &#8212; the majority of these wind vectors had height assignments within the 900-990 hPa range, indicating that the circulation was located above the surface. The highest DMW speed was 36 knots.<\/p>\n<div style=\"width: 653px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/02\/210202_goes16_visible_derivedMotionWinds_NortheastUS_low_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/02\/neus_dmw_vis-20210202_141021.png\" alt=\"GOES-16 &quot;Red&quot; Visible (0.6 \u00b5m) images, with plots of Derived Motion Winds [click to play animation | MP4]\" width=\"643\" height=\"300\" \/><\/a><p class=\"wp-caption-text\">GOES-16 &#8220;Red&#8221; Visible (0.6 \u00b5m) images, with plots of Derived Motion Winds [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/02\/210202_goes16_visible_derivedMotionWinds_NortheastUS_low_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>GOES-16 (GOES-East) Mid-level Water Vapor (6.9 \u00b5m) images with plots of hourly surface weather type (above) showed the formation of a well-defined cold conveyor belt that moved westward across parts of the Northeast US during the 01 February &#8211; 02 February 2021 period. This moist airstream helped to enhance snowfall rates, with 2-4 inches per [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":39786,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[74,25,5],"tags":[],"class_list":["post-39783","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-goes-16","category-satellite-winds","category-winter-weather"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/39783","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\/18"}],"replies":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/comments?post=39783"}],"version-history":[{"count":13,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/39783\/revisions"}],"predecessor-version":[{"id":39823,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/39783\/revisions\/39823"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/39786"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=39783"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=39783"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=39783"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}