{"id":7395,"date":"2011-01-13T18:59:48","date_gmt":"2011-01-13T18:59:48","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=7395"},"modified":"2011-01-25T17:53:03","modified_gmt":"2011-01-25T17:53:03","slug":"northeast-us-winter-storm","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/7395","title":{"rendered":"Northeast US winter storm"},"content":{"rendered":"<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2011\/01\/110112_g13_wv_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"GOES-13 6.5 \u00c2\u00b5m water vapor images (click image to play animation)\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2011\/01\/US_Water_Vapor_20110112_1745.png\" alt=\"GOES-13 6.5 \u00c2\u00b5m water vapor images (click image to play animation)\" width=\"480\" height=\"459\" \/><\/a><p class=\"wp-caption-text\">GOES-13 6.5 \u00c2\u00b5m water vapor images (click image to play animation)<\/p><\/div>\n<p>A strong &#8220;Nor&#8217;easter&#8221; winter storm impacted much of the northeastern US on <strong><a title=\"12 January 2011 daily weather map\" href=\"http:\/\/www.hpc.ncep.noaa.gov\/dailywxmap\/index_20110112.html\">12 January<\/a> &#8211;<a title=\"13 January 2011 daily weather map\" href=\"http:\/\/www.hpc.ncep.noaa.gov\/dailywxmap\/index_20110113.html\"> 13 January 2011<\/a><\/strong>. The storm exhibited a nice presentation on AWIPS images of the GOES-13 6.5 \u00c2\u00b5m &#8220;water vapor channel&#8221; data <em><strong>(above; click image to play animation)<\/strong><\/em>. Storm total snowfall amounts included <strong>36.0 inches<\/strong> at Wilmington, Vermont, <strong>34.5 inches<\/strong> at Savoy, Massachusetts, and<strong> 29.5 inches<\/strong> at North Haven, Connecticut (<a title=\"HPC Storm Summary\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2011\/01\/110109-13_hpc_storm_summary.text\"><strong>HPC Storm Summary<\/strong><\/a>).<\/p>\n<p>A comparison of the GOES-13 6.5 \u00c2\u00b5m water vapor image at 18:15 UTC and the corresponding <strong><a title=\"MODIS in AWIPS: VISIT training lesson\" href=\"http:\/\/rammb.cira.colostate.edu\/training\/visit\/training_sessions\/modis_products_in_awips\/\">MODIS<\/a><\/strong> 6.7 \u00c2\u00b5m water vapor image at 18:16 UTC <em><strong>(below)<\/strong><\/em> demonstrates the value of better spatial resolution <em>(1 km on the MODIS image)<\/em> for depicting subtle storm structures. Also note the slight northwestward &#8220;parallax shift&#8221; of the features on the GOES-13 image, due to the large viewing angle from GOES-13<em> (which is positioned over the Equator at 75\u00c2\u00ba West longitude)<\/em>.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2011\/01\/110112_modis_goes_wv_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"MODIS 6.7 \u00c2\u00b5m and GOES-13 6.5 \u00c2\u00b5m water vapor channel images\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2011\/01\/110112_modis_goes_wv_anim.gif\" alt=\"MODIS 6.7 \u00c2\u00b5m and GOES-13 6.5 \u00c2\u00b5m water vapor channel images\" width=\"480\" height=\"459\" \/><\/a><p class=\"wp-caption-text\">MODIS 6.7 \u00c2\u00b5m and GOES-13 6.5 \u00c2\u00b5m water vapor channel images<\/p><\/div>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2011\/01\/110112_g13_wv_pv1.5_xsec.jpg\"><img loading=\"lazy\" decoding=\"async\" title=\"GOES-13 water vapor + RUC80 PV1.5 pressure + Cross Section line\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2011\/01\/110112_g13_wv_pv1.5_xsec.jpg\" alt=\"GOES-13 water vapor + RUC80 PV1.5 pressure + Cross Section line\" width=\"480\" height=\"408\" \/><\/a><p class=\"wp-caption-text\">GOES-13 water vapor + RUC80 PV1.5 pressure + Cross Section line<\/p><\/div>\n<p>There was a strong Potential Vorticity (PV) anomaly associated with this storm &#8212; in fact, a northwest-to-southeast oriented cross section of RUC80 model fields through the developing &#8220;comma structure&#8221; seen on GOES-13 water vapor imagery at 15 UTC\u00c2\u00a0 <em><strong>(above)<\/strong><\/em> showed that the tropopause <em>(taken to be the pressure of the PV1.5 surface)<\/em> had been drawn downward to near the 800 hPa pressure level <em><strong>(below)<\/strong><\/em>.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2011\/01\/RUC80_lineA__Pot_Vorticity_20110112_1500F000.png\"><img loading=\"lazy\" decoding=\"async\" title=\"RUC80 model cross section\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2011\/01\/RUC80_lineA__Pot_Vorticity_20110112_1500F000.png\" alt=\"RUC80 model cross section\" width=\"480\" height=\"459\" \/><\/a><p class=\"wp-caption-text\">RUC80 model cross section<\/p><\/div>\n<p>A sequence of 1-km resolution MODIS 11.0 \u00c2\u00b5m IR and <strong><a title=\"POES\/AVHRR in AWIPS: VISIT training lesson\" href=\"http:\/\/rammb.cira.colostate.edu\/training\/visit\/training_sessions\/poes_and_avhrr_satellite_products_in_awips\/\">POES AVHRR<\/a><\/strong> 10.8 \u00c2\u00b5m IR image<em><strong> (below)<\/strong><\/em> showed the development of banding features with IR brightness temperatures as cold as -50 to -60\u00c2\u00ba C <em>(orange to red color enhancement)<\/em>.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2011\/01\/110112_modis_avhrr_ir_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"MODIS 11.0 \u00c2\u00b5m and POES AVHRR 10.8 \u00c2\u00b5m IR images\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2011\/01\/110112_modis_avhrr_ir_anim.gif\" alt=\"MODIS 11.0 \u00c2\u00b5m and POES AVHRR 10.8 \u00c2\u00b5m IR images\" width=\"480\" height=\"459\" \/><\/a><p class=\"wp-caption-text\">MODIS 11.0 \u00c2\u00b5m and POES AVHRR 10.8 \u00c2\u00b5m IR images<\/p><\/div>\n<p>After the storm departed, a comparison of a 13 January MODIS 0.65 \u00c2\u00b5m visible channel image with the corresponding MODIS Red\/Green\/Blue (RGB) image &#8212; created using MODIS channels 01\/07\/07 &#8212; showed the extent of some of the snow cover <em>(which appears as the darkest shades of red on the RGB image),<\/em> as well as the presence of supercooled water droplet clouds and glaciated ice crystal clouds <em>(which show up as light gray\u00c2\u00a0and lighter shades of red on the RGB image, respectively)<\/em>.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2011\/01\/110113_modis_vis_rgb_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"MODIS 0.65 \u00c2\u00b5m visible image + MODIS false-color Red\/Green\/Blue (RGB) image\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2011\/01\/110113_modis_vis_rgb_anim.gif\" alt=\"MODIS 0.65 \u00c2\u00b5m visible image + MODIS false-color Red\/Green\/Blue (RGB) image\" width=\"480\" height=\"459\" \/><\/a><p class=\"wp-caption-text\">MODIS 0.65 \u00c2\u00b5m visible image + MODIS false-color Red\/Green\/Blue (RGB) image<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>A strong &#8220;Nor&#8217;easter&#8221; winter storm impacted much of the northeastern US on 12 January &#8211; 13 January 2011. The storm exhibited a nice presentation on AWIPS images of the GOES-13 6.5 \u00c2\u00b5m &#8220;water vapor channel&#8221; data (above; click image to play animation). Storm total snowfall amounts included 36.0 inches at Wilmington, Vermont, 34.5 inches at [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[22,11,12,26,45,5],"tags":[],"class_list":["post-7395","post","type-post","status-publish","format-standard","hentry","category-avhrr","category-goes-13","category-modis","category-poes","category-redgreenblue-rgb-images","category-winter-weather"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/7395","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=7395"}],"version-history":[{"count":12,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/7395\/revisions"}],"predecessor-version":[{"id":7510,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/7395\/revisions\/7510"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=7395"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=7395"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=7395"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}