{"id":39739,"date":"2021-01-23T23:59:08","date_gmt":"2021-01-23T23:59:08","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=39739"},"modified":"2021-01-27T04:14:00","modified_gmt":"2021-01-27T04:14:00","slug":"heavy-rainfall-and-snowfall-in-southern-california","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/39739","title":{"rendered":"Heavy rainfall and snowfall in Southern California"},"content":{"rendered":"<p><div style=\"width: 655px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/01\/210123_goes17_airMassRGB_pv1.5pressure_Southern_California_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/01\/socal_rgb-20210123_180117.png\" alt=\"GOES-17 Air Mass RGB images, with contours of PV1.5 pressure [click to play animation | MP4]\" width=\"645\" height=\"301\" \/><\/a><p class=\"wp-caption-text\">GOES-17 Air Mass RGB images, with contours of PV1.5 pressure [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/01\/210123_goes17_airMassRGB_pv1.5pressure_Southern_California_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>As an <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/01\/210123_210124_500hPa_height_anomaly_anim.gif\"><strong>anomalously-deep<\/strong><\/a> 500 hPa low began to move inland over Southern California during the <a href=\"https:\/\/www.wpc.ncep.noaa.gov\/dailywxmap\/index_20210123.html\"><strong>23 January<\/strong><\/a> &#8211; <a href=\"https:\/\/www.wpc.ncep.noaa.gov\/dailywxmap\/index_20210124.html\"><strong>24 January 2021<\/strong><\/a> period, GOES-17 <em>(GOES-West)<\/em>\u00a0 <a href=\"http:\/\/rammb.cira.colostate.edu\/training\/visit\/quick_guides\/QuickGuide_GOESR_AirMassRGB_final.pdf\"><strong>Air Mass RGB<\/strong><\/a> images<em><strong>\u00a0(above)<\/strong><\/em> showed a compact Potential Vorticity (PV) anomaly approaching the coast &#8212; and the RAP40 model indicated that the &#8220;dynamic tropopause&#8221; (defined here as the pressure of the PV1.5 surface) was descending to the 675 hPa pressure level at <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/01\/socal_rgb-20210123_180117.png\"><strong>18 UTC<\/strong><\/a>.<\/p>\n<p>A west-to-east oriented cross section of RAP40 model fields along Line A-A&#8217; <em><strong>(below)<\/strong> <\/em>depicted the descending dynamic tropopause at 19 UTC.<\/p>\n<p><div style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/01\/210123_19utc_ruc40_lineA_cross_section.png\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/01\/210123_19utc_ruc40_lineA_cross_section.png\" alt=\"Cross section of RAP40 model fields along line A-A' [click to enlarge]\" width=\"640\" height=\"300\" \/><\/a><p class=\"wp-caption-text\">Cross section of RAP40 model fields along line A-A&#8217; [click to enlarge]<\/p><\/div>GOES-17 Mid-level Water Vapor (<a href=\"http:\/\/cimss.ssec.wisc.edu\/goes\/OCLOFactSheetPDFs\/ABIQuickGuide_Band09.pdf\"><strong>6.9 \u00b5m<\/strong><\/a>) images <em><strong>(below)<\/strong><\/em> showed the increasing reports of rain and snow that resulted as the PV Anomaly moved inland and provided additional forcing for ascent. Near the coast, thunderstorms were reported at <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/01\/210123_KFUL_SFCMG.GIF\"><strong>Fulton<\/strong><\/a> and <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/01\/210123_KLGB_SFCMG.GIF\"><strong>Long Beach<\/strong><\/a> around 03 UTC. <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/01\/210124_ksgx_precip_summary.text\"><strong>Storm total precipitation<\/strong><\/a> amounts included rainfall of 1.40 inch and snowfall of 12-18 inches.<\/p>\n<p><div style=\"width: 651px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/01\/210123_goes17_waterVapor_SoCal_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/01\/G17_WV_WX1_CA_RAIN_SNOW_23JAN2021_B9_2021024_030117_GOES-17_0001PANEL_FRAME0000145.GIF\" alt=\"GOES-17 Mid-level Water Vapor (6.9 \u00b5m) images, with plots of hourly surface weather type [click to play animation | MP4]\" width=\"641\" height=\"480\" \/><\/a><p class=\"wp-caption-text\">GOES-17 Mid-level Water Vapor <em>(6.9 \u00b5m)<\/em> images, with plots of hourly surface weather type [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/01\/210123_goes17_waterVapor_SoCal_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>GOES-17 Water Vapor images at 2301 UTC and 0246 UTC <em><strong>(below)<\/strong><\/em> revealed sporadic lightning activity (indicated by small clusters of <a href=\"https:\/\/www.goes-r.gov\/spacesegment\/glm.html\"><strong>GLM<\/strong><\/a> Groups).<\/p>\n<p><div style=\"width: 656px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/01\/G17_WV_GLM_CA_23JAN2021_B9_2021023_230117_GOES-17_0001PANEL_FRAME0000097.GIF\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/01\/G17_WV_GLM_CA_23JAN2021_B9_2021023_230117_GOES-17_0001PANEL_FRAME0000097.GIF\" alt=\"GOES-17 Mid-level Water Vapor (6.9 \u00b5m) image at 2301 UTC, with GLM Groups plotted in red [click to enlarge]\" width=\"646\" height=\"485\" \/><\/a><p class=\"wp-caption-text\">GOES-17 Mid-level Water Vapor <em>(6.9 \u00b5m)<\/em> image at 2301 UTC, with GLM Groups plotted in red [click to enlarge]<\/p><\/div><div style=\"width: 653px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/01\/G17_WV_GLM_CA_23JAN2021_B9_2021024_024617_GOES-17_0001PANEL_FRAME0000142.GIF\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/01\/G17_WV_GLM_CA_23JAN2021_B9_2021024_024617_GOES-17_0001PANEL_FRAME0000142.GIF\" alt=\"GOES-17 Mid-level Water Vapor (6.9 \u00b5m) image at 0246 UTC, with GLM Groups plotted in red [click to enlarge]\" width=\"643\" height=\"482\" \/><\/a><p class=\"wp-caption-text\">GOES-17 Mid-level Water Vapor<em> (6.9 \u00b5m)<\/em> image at 0246 UTC, with GLM Groups plotted in red [click to enlarge]<\/p><\/div><center><\/center><\/p>\n<p style=\"text-align: center;\"><strong>===== 24 January Update =====<\/strong><\/p>\n<p><div style=\"width: 655px\" class=\"wp-caption aligncenter\"><a class=\"thumbnail\" href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/01\/210124_goes17_daySnowFogRGB_SoCal_anim.gif\"><img loading=\"lazy\" decoding=\"async\" class=\"thumbnail\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/01\/socal_snow-20210124_171117.png\" alt=\"GOES-17 Day Snow-Fog RGB images [click t play animation | MP4]\" width=\"645\" height=\"302\" \/><\/a><p class=\"wp-caption-text\">GOES-17 Day Snow-Fog RGB images [click to play animation | <a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/01\/210124_goes17_daySnowFogRGB_SoCal_anim.mp4\"><strong>MP4<\/strong><\/a>]<\/p><\/div>On the following day, as clouds began to clear the areal extent of resulting fresh snow cover\u00a0<em>(darker shades of red)<\/em> was seen in GOES-17 <a href=\"http:\/\/rammb.cira.colostate.edu\/training\/visit\/quick_guides\/QuickGuide_DaySnowFogRGB_final_v2.pdf\"><strong>Day Snow-Fog RGB<\/strong><\/a> images <em><strong>(above)<\/strong><\/em>. Even parts of the high desert &#8212; north and east of the mountain ranges &#8212; received some snowfall (for example, 2-3 inches were reported at Hesperia).<\/p>\n<p>Suomi NPP VIIRS True Color RGB and False Color RGB images<em><strong> (below)<\/strong> <\/em>showed the snow cover <em>(shades of cyan)<\/em> at 2036 UTC.<\/p>\n<div style=\"width: 655px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/01\/210124_2036utc_suomiNPP_viirs_trueColorRGB_SoCal_anim.gif\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/images\/2021\/01\/210124_2036utc_suomiNPP_viirs_trueColorRGB_SoCal_anim.gif\" alt=\"Suomi NPP VIIRS True Color RGB and False Color RGB images [click to enlarge]\" width=\"645\" height=\"301\" \/><\/a><p class=\"wp-caption-text\">Suomi NPP VIIRS True Color RGB and False Color RGB images [click to enlarge]<\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>As an anomalously-deep 500 hPa low began to move inland over Southern California during the 23 January &#8211; 24 January 2021 period, GOES-17 (GOES-West)\u00a0 Air Mass RGB images\u00a0(above) showed a compact Potential Vorticity (PV) anomaly approaching the coast &#8212; and the RAP40 model indicated that the &#8220;dynamic tropopause&#8221; (defined here as the pressure of the [&hellip;]<\/p>\n","protected":false},"author":18,"featured_media":39745,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[76,80,16,30,45,49,48,5],"tags":[],"class_list":["post-39739","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-glm","category-goes-17","category-heavy-rain-flooding","category-lightning","category-redgreenblue-rgb-images","category-suomi_npp","category-viirs","category-winter-weather"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/39739","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=39739"}],"version-history":[{"count":5,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/39739\/revisions"}],"predecessor-version":[{"id":39746,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/39739\/revisions\/39746"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/39745"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=39739"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=39739"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=39739"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}