{"id":15047,"date":"2014-02-28T23:59:40","date_gmt":"2014-02-28T23:59:40","guid":{"rendered":"http:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=15047"},"modified":"2014-03-03T02:22:13","modified_gmt":"2014-03-03T02:22:13","slug":"strong-storm-off-the-coast-of-california","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/15047","title":{"rendered":"Strong storm off the coast of California"},"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\/2014\/02\/140227-28_g15_wv_CA_storm_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"GOES-15 6.5 \u00c2\u00b5m water vapor channel images (click to play animation)\" alt=\"GOES-15 6.5 \u00c2\u00b5m water vapor channel images (click to play animation)\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/02\/140227-28_G15_WV_CA_STORM_040.GIF\" width=\"480\" height=\"360\" \/><\/a><p class=\"wp-caption-text\">GOES-15 6.5 \u00c2\u00b5m water vapor channel images (click to play animation)<\/p><\/div>\n<p>McIDAS images of 4-km resolution GOES-15 6.5 \u00c2\u00b5m water vapor channel data <em><strong>(above; click image to play animation; also available as an <a title=\"MP4 animation of GOES-15 water vapor images\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/02\/140227-28_g15_wv_CA_storm_anim.mp4\">MP4 animation<\/a>)<\/strong><\/em> showed the development of a strong and rapidly-occluding storm off the coast of California during the <a title=\"27 February 2014 daily weather map\" href=\"http:\/\/www.hpc.ncep.noaa.gov\/dailywxmap\/index_20140227.html\"><strong>27 February<\/strong><\/a> &#8211; <a title=\"28 February 2014 daily weather map\" href=\"http:\/\/www.hpc.ncep.noaa.gov\/dailywxmap\/index_20140228.html\"><strong>28 February 2014<\/strong><\/a> period.<\/p>\n<p>An AWIPS image of 17:30 UTC GOES-15 water vapor channel data with overlays of 17:28 UTC Metop ASCAT surface scatterometer winds and the 18:00 UTC tropical surface analysis <em><strong>(below)<\/strong><\/em> showed satellite-sensed surface winds as strong as 51 knots in the southwestern quadrant of the storm.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/02\/140228_1728z_ascat_winds_CA_storm_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"GOES-15 6.5 \u00c2\u00b5m water vapor channel image with ASCAT surface scatterometer winds and surface analysis\" alt=\"GOES-15 6.5 \u00c2\u00b5m water vapor channel image with ASCAT surface scatterometer winds and surface analysis\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/02\/140228_1728z_ascat_winds_CA_storm_anim.gif\" width=\"480\" height=\"345\" \/><\/a><p class=\"wp-caption-text\">GOES-15 6.5 \u00c2\u00b5m water vapor channel image with ASCAT surface scatterometer winds and surface analysis<\/p><\/div>\n<p>Greater detail in the storm structure could be seen in 1-km resolution MODIS 6.7 \u00c2\u00b5m water vapor channel images at 10:32 UTC and 21:40 UTC <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\/2014\/02\/140228_modis_wv_CA_storm_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"MODIS 6.7 \u00c2\u00b5m water vapor channel images\" alt=\"MODIS 6.7 \u00c2\u00b5m water vapor channel images\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/02\/140228_modis_wv_CA_storm_anim.gif\" width=\"480\" height=\"357\" \/><\/a><p class=\"wp-caption-text\">MODIS 6.7 \u00c2\u00b5m water vapor channel images<\/p><\/div>\n<p>One indication of the strength of the storm was the high amounts of GOES-15 sounder Total Column Ozone associated with the circulation <em><strong>(below; click image to play animation),<\/strong><\/em> which reached levels as high as 440-450 Dobson Units <em>(lighter red color enhancement)<\/em>. Such high levels of total column ozone are also often associated with potential vorticity anomalies and a dramatically lowered tropopause &#8212; in this case, the GFS40 model indicated the the dynamic tropopause <em>(taken to be the pressure of the PV1.5 surface)<\/em> was as <a title=\"GFS40 model fields of PV1.5 pressure and 500 hPa geopotential height\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/02\/GFS40_PV15_Pressure_20140228_1800F000.png\"><strong>below the 480 hPa pressure level<\/strong><\/a> at 18:00 UTC. It is interesting to note that there was a <a title=\"pilot report of moderate turbulence\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/02\/140228_18z_g15_sounder_ozone_pirep.jpg\"><strong>pilot report of moderate turbulence at 36,000 feet<\/strong><\/a>, along the sharp western gradient of the total column ozone (and the sharp gradient of the PV1.5 pressure) &#8212; the pilot noted that the turbulene lasted for 10 minutes.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/02\/140228_g15_sounder_ozone_CA_storm_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"GOES-15 sounder Total Column Ozone product (click to play animation)\" alt=\"GOES-15 sounder Total Column Ozone product (click to play animation)\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/02\/GOES_Ozone_20140228_1200.png\" width=\"480\" height=\"357\" \/><\/a><p class=\"wp-caption-text\">GOES-15 sounder Total Column Ozone product (click to play animation)<\/p><\/div>\n<p>A comparison of 375-meter resolution Suomi NPP VIIRS 0.64 \u00c2\u00b5m visible channel and 11.45 \u00c2\u00b5m IR channel images at 22:08 UTC <em><strong>(below)<\/strong><\/em> revealed a few convective elements offshore which exhibited cloud-top IR brightness temperatures as cold as -50\u00c2\u00ba C <em>(yellow color enhancement),<\/em> with a few cloud-to-ground lightning strikes being detected.<\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/02\/140228_2208z_suomi_npp_viirs_visible_ir_CA_storm_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"Suomi NPP VIIRS 0.64 \u00c2\u00b5m visible channel and 11.45 \u00c2\u00b5m IR channel images (with cloud-to-ground lightning strikes)\" alt=\"Suomi NPP VIIRS 0.64 \u00c2\u00b5m visible channel and 11.45 \u00c2\u00b5m IR channel images (with cloud-to-ground lightning strikes)\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/02\/140228_2208z_suomi_npp_viirs_visible_ir_CA_storm_anim.gif\" width=\"480\" height=\"357\" \/><\/a><p class=\"wp-caption-text\">Suomi NPP VIIRS 0.64 \u00c2\u00b5m visible channel and 11.45 \u00c2\u00b5m IR channel images (with cloud-to-ground lightning strikes)<\/p><\/div>\n<p style=\"text-align: center;\"><strong>===== 01 March Update =====<\/strong><\/p>\n<div style=\"width: 490px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/03\/140301_1022z_suomi_npp_viirs_dnb_ir_CA_storm_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"Suomi NPP VIIRS 0.7 \u00c2\u00b5m Day\/Night Band and 11.45 \u00c2\u00b5m IR channel images\" alt=\"Suomi NPP VIIRS 0.7 \u00c2\u00b5m Day\/Night Band and 11.45 \u00c2\u00b5m IR channel images\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/03\/140301_1022z_suomi_npp_viirs_dnb_ir_CA_storm_anim.gif\" width=\"480\" height=\"325\" \/><\/a><p class=\"wp-caption-text\">Suomi NPP VIIRS 0.7 \u00c2\u00b5m Day\/Night Band and 11.45 \u00c2\u00b5m IR channel images<\/p><\/div>\n<p>A comparison of Suomi NPP VIIRS 0.7 \u00c2\u00b5m Day\/Night Band (DNB) and 11.45 \u00c2\u00b5m IR channel images at 10:22 UTC or 2:22 AM local time on <a title=\"01 March 2014 daily weather map\" href=\"http:\/\/www.hpc.ncep.noaa.gov\/dailywxmap\/index_20140301.html\"><strong>01 March<\/strong><\/a> <em><strong>(above)<\/strong><\/em> revealed the presence of numerous arc-shaped mesospheric airglow waves in the western semicircle of the storm circulation on the DNB image &#8212; note that there was no corresponding wave signature on the IR image.<\/p>\n<p>These vertically-propagating mesospheric airglow waves were likely generated by the 140-knot jet streak that was moving southward around the rear side of the storm\u00c2\u00a0 <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\/2014\/03\/140301_1022z_suomi_npp_viirs_dnb_CA_storm_nam_250_winds_anim.gif\"><img loading=\"lazy\" decoding=\"async\" title=\"Suomi NPP VIIRS 0.7 \u00c2\u00b5m Day\/Night Band image with NAM 250 hPa winds and isotachs\" alt=\"Suomi NPP VIIRS 0.7 \u00c2\u00b5m Day\/Night Band image with NAM 250 hPa winds and isotachs\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2014\/03\/140301_1022z_suomi_npp_viirs_dnb_CA_storm_nam_250_winds_anim.gif\" width=\"480\" height=\"325\" \/><\/a><p class=\"wp-caption-text\">Suomi NPP VIIRS 0.7 \u00c2\u00b5m Day\/Night Band image with NAM 250 hPa winds and isotachs<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>McIDAS images of 4-km resolution GOES-15 6.5 \u00c2\u00b5m water vapor channel data (above; click image to play animation; also available as an MP4 animation) showed the development of a strong and rapidly-occluding storm off the coast of California during the 27 February &#8211; 28 February 2014 period. An AWIPS image of 17:30 UTC GOES-15 water [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":15048,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[21,15,43,30,58,12,25,49,48],"tags":[],"class_list":["post-15047","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-aviation","category-goes-sounder","category-goes-15","category-lightning","category-metop","category-modis","category-satellite-winds","category-suomi_npp","category-viirs"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/15047","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=15047"}],"version-history":[{"count":7,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/15047\/revisions"}],"predecessor-version":[{"id":15056,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/15047\/revisions\/15056"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/15048"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=15047"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=15047"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=15047"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}