{"id":461,"date":"2013-12-05T22:26:00","date_gmt":"2013-12-05T22:26:00","guid":{"rendered":"http:\/\/rammb.cira.colostate.edu\/research\/goes-r\/proving_ground\/blog\/?p=461"},"modified":"2026-03-06T09:05:41","modified_gmt":"2026-03-06T16:05:41","slug":"widespread-fog-east-of-the-rockies-3-dec-2013","status":"publish","type":"post","link":"https:\/\/rammb2.cira.colostate.edu\/proving-ground-blog\/2013\/12\/05\/widespread-fog-east-of-the-rockies-3-dec-2013\/","title":{"rendered":"Widespread Fog East of the Rockies &#8211; 3 Dec 2013"},"content":{"rendered":"\n<p>Widespread fog and low clouds covered much of the nation east of the Rockies 0n the morning of 3 Dec in the moist airmass ahead of the developing western storm and strong cold front that has since pushed south. &nbsp;Dense Fog Advisories were issued by many WFOs, as seen in the graphic below valid at 1324 UTC on 3 Dec.<\/p>\n\n\n\n<figure class=\"wp-block-image alignleft\"><a href=\"https:\/\/rammb2.cira.colostate.edu\/proving-ground-blog\/wp-content\/uploads\/sites\/6\/2013\/12\/FOG2013.jpg\" rel=\"attachment wp-att-463\"><img loading=\"lazy\" decoding=\"async\" width=\"815\" height=\"741\" src=\"https:\/\/rammb2.cira.colostate.edu\/proving-ground-blog\/wp-content\/uploads\/sites\/6\/2013\/12\/FOG2013.jpg\" alt=\"surface weather map at 1300 UTC on 3 Dec \" class=\"wp-image-463\" srcset=\"https:\/\/rammb2.cira.colostate.edu\/proving-ground-blog\/wp-content\/uploads\/sites\/6\/2013\/12\/FOG2013.jpg 815w, https:\/\/rammb2.cira.colostate.edu\/proving-ground-blog\/wp-content\/uploads\/sites\/6\/2013\/12\/FOG2013-300x273.jpg 300w, https:\/\/rammb2.cira.colostate.edu\/proving-ground-blog\/wp-content\/uploads\/sites\/6\/2013\/12\/FOG2013-768x698.jpg 768w\" sizes=\"auto, (max-width: 815px) 100vw, 815px\" \/><\/a><figcaption class=\"wp-element-caption\">NWS Watches and Warnings as of 1324 UTC on 3 Dec 2013<\/figcaption><\/figure>\n\n\n\n<p>The surface weather map at 1300 UTC on 3 Dec is shown below. &nbsp;A complex storm system is taking shape in the Rockies while an Arctic high pushes cold air southward into the Northern Plains.<\/p>\n\n\n\n<figure class=\"wp-block-image alignleft\"><a href=\"https:\/\/rammb2.cira.colostate.edu\/proving-ground-blog\/wp-content\/uploads\/sites\/6\/2013\/12\/stnplot_201312031.gif\" rel=\"attachment wp-att-477\"><img loading=\"lazy\" decoding=\"async\" width=\"1088\" height=\"783\" src=\"https:\/\/rammb2.cira.colostate.edu\/proving-ground-blog\/wp-content\/uploads\/sites\/6\/2013\/12\/stnplot_201312031.gif\" alt=\"Surface analysis and plot at 1300 UTC on 3 Dec 2013.\" class=\"wp-image-477\"\/><\/a><figcaption class=\"wp-element-caption\">Surface analysis and plot at 1300 UTC on 3 Dec 2013.<\/figcaption><\/figure>\n\n\n\n<p>A closer look at the observations is given in the plot below. &nbsp;In this plot visibility is given below the station circle, weather to the right, and ceiling height (feet, AGL) to the left. Note the large number of stations reported low visibilities due to fog. &nbsp;East of the dense fog area was a huge area with more scattered fog reports but widespread low overcast conditions.<\/p>\n\n\n\n<figure class=\"wp-block-image alignleft\"><a href=\"https:\/\/rammb2.cira.colostate.edu\/proving-ground-blog\/wp-content\/uploads\/sites\/6\/2013\/12\/METARobs_plot_v12z3Dec131.jpg\" rel=\"attachment wp-att-466\"><img loading=\"lazy\" decoding=\"async\" width=\"1522\" height=\"1077\" src=\"https:\/\/rammb2.cira.colostate.edu\/proving-ground-blog\/wp-content\/uploads\/sites\/6\/2013\/12\/METARobs_plot_v12z3Dec131.jpg\" alt=\"METAR station plot of weather, ceiling and visibility at 1200 UTC on 3 Dec.\" class=\"wp-image-466\" srcset=\"https:\/\/rammb2.cira.colostate.edu\/proving-ground-blog\/wp-content\/uploads\/sites\/6\/2013\/12\/METARobs_plot_v12z3Dec131.jpg 1522w, https:\/\/rammb2.cira.colostate.edu\/proving-ground-blog\/wp-content\/uploads\/sites\/6\/2013\/12\/METARobs_plot_v12z3Dec131-300x212.jpg 300w, https:\/\/rammb2.cira.colostate.edu\/proving-ground-blog\/wp-content\/uploads\/sites\/6\/2013\/12\/METARobs_plot_v12z3Dec131-1024x725.jpg 1024w, https:\/\/rammb2.cira.colostate.edu\/proving-ground-blog\/wp-content\/uploads\/sites\/6\/2013\/12\/METARobs_plot_v12z3Dec131-768x543.jpg 768w\" sizes=\"auto, (max-width: 1522px) 100vw, 1522px\" \/><\/a><figcaption class=\"wp-element-caption\">METAR station plot of weather, ceiling and visibility at 1200 UTC on 3 Dec.<\/figcaption><\/figure>\n\n\n\n<p>CIRA has two types of overview imagery that make fog and low clouds easier to see, and both will be available in improved versions in the GOES-R era. &nbsp;Below we see an example of GeoColor imagery, one version with night lights and the other without, both for 1145 UTC on 3 Dec. &nbsp;In this imagery low clouds and fog appear in red\/pink tones, while clouds or snow cover are white. &nbsp;Much of North America east of the Rockies is covered by low clouds and fog,&nbsp;interrupted&nbsp;in the imagery in some areas by higher clouds. &nbsp;GeoColor imagery is intended as a general overview type of satellite imagery.<\/p>\n\n\n\n<figure class=\"wp-block-image alignleft\"><a href=\"https:\/\/rammb2.cira.colostate.edu\/proving-ground-blog\/wp-content\/uploads\/sites\/6\/2013\/12\/geocolorimages.jpg\" rel=\"attachment wp-att-469\"><img loading=\"lazy\" decoding=\"async\" width=\"1068\" height=\"620\" src=\"https:\/\/rammb2.cira.colostate.edu\/proving-ground-blog\/wp-content\/uploads\/sites\/6\/2013\/12\/geocolorimages.jpg\" alt=\"GeoColor imagery all clouds other than low clouds (or fog) appear white. \" class=\"wp-image-469\" srcset=\"https:\/\/rammb2.cira.colostate.edu\/proving-ground-blog\/wp-content\/uploads\/sites\/6\/2013\/12\/geocolorimages.jpg 1068w, https:\/\/rammb2.cira.colostate.edu\/proving-ground-blog\/wp-content\/uploads\/sites\/6\/2013\/12\/geocolorimages-300x174.jpg 300w, https:\/\/rammb2.cira.colostate.edu\/proving-ground-blog\/wp-content\/uploads\/sites\/6\/2013\/12\/geocolorimages-1024x594.jpg 1024w, https:\/\/rammb2.cira.colostate.edu\/proving-ground-blog\/wp-content\/uploads\/sites\/6\/2013\/12\/geocolorimages-768x446.jpg 768w\" sizes=\"auto, (max-width: 1068px) 100vw, 1068px\" \/><\/a><\/figure>\n\n\n\n<p><\/p>\n\n\n\n<p>In the GeoColor imagery all clouds other than low clouds (or fog) appear white. &nbsp;Another type of imagery (called Low-cloud\/fog imagery) is designed to highlight low clouds and fog in a whitish color both during the night and during the day, but also colors higher clouds thereby giving more information about them. &nbsp;An image also for 1145 UTC is shown below. &nbsp;Note that thin cirrus appears as black during nighttime imagery, and we see that there are areas of thin cirrus covering some of the regions of low clouds and fog.<\/p>\n\n\n\n<figure class=\"wp-block-image alignleft\"><a href=\"https:\/\/rammb2.cira.colostate.edu\/proving-ground-blog\/wp-content\/uploads\/sites\/6\/2013\/12\/goese_lcfog_20131203114500.gif\" rel=\"attachment wp-att-470\"><img loading=\"lazy\" decoding=\"async\" width=\"640\" height=\"480\" src=\"https:\/\/rammb2.cira.colostate.edu\/proving-ground-blog\/wp-content\/uploads\/sites\/6\/2013\/12\/goese_lcfog_20131203114500.gif\" alt=\"CIRA Low-cloud\/fog imagery for 1145 UTC on 3 Dec.\" class=\"wp-image-470\"\/><\/a><figcaption class=\"wp-element-caption\">CIRA Low-cloud\/fog imagery for 1145 UTC on 3 Dec.<\/figcaption><\/figure>\n","protected":false},"excerpt":{"rendered":"<p>Widespread fog and low clouds covered much of the nation east of the Rockies 0n the morning of 3 Dec in the moist airmass ahead of the developing western storm and strong cold front that has since pushed south. &nbsp;Dense Fog Advisories were issued by many WFOs, as seen in the graphic below valid at [&hellip;]<\/p>\n","protected":false},"author":6,"featured_media":0,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1],"tags":[],"class_list":["post-461","post","type-post","status-publish","format-standard","hentry","category-uncategorized"],"_links":{"self":[{"href":"https:\/\/rammb2.cira.colostate.edu\/proving-ground-blog\/wp-json\/wp\/v2\/posts\/461","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/rammb2.cira.colostate.edu\/proving-ground-blog\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/rammb2.cira.colostate.edu\/proving-ground-blog\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/rammb2.cira.colostate.edu\/proving-ground-blog\/wp-json\/wp\/v2\/users\/6"}],"replies":[{"embeddable":true,"href":"https:\/\/rammb2.cira.colostate.edu\/proving-ground-blog\/wp-json\/wp\/v2\/comments?post=461"}],"version-history":[{"count":2,"href":"https:\/\/rammb2.cira.colostate.edu\/proving-ground-blog\/wp-json\/wp\/v2\/posts\/461\/revisions"}],"predecessor-version":[{"id":1274,"href":"https:\/\/rammb2.cira.colostate.edu\/proving-ground-blog\/wp-json\/wp\/v2\/posts\/461\/revisions\/1274"}],"wp:attachment":[{"href":"https:\/\/rammb2.cira.colostate.edu\/proving-ground-blog\/wp-json\/wp\/v2\/media?parent=461"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/rammb2.cira.colostate.edu\/proving-ground-blog\/wp-json\/wp\/v2\/categories?post=461"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/rammb2.cira.colostate.edu\/proving-ground-blog\/wp-json\/wp\/v2\/tags?post=461"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}