{"id":69479,"date":"2026-03-17T21:13:17","date_gmt":"2026-03-17T21:13:17","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=69479"},"modified":"2026-03-17T21:13:17","modified_gmt":"2026-03-17T21:13:17","slug":"intense-cyclone-causes-massive-dust-advection-over-mediterranean","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/69479","title":{"rendered":"Intense Cyclone Causes Massive Dust Advection Over Mediterranean"},"content":{"rendered":"\n<p>Just north of Libya on the afternoon of 17 March 2026, a large cyclone can be seen forcing a significant amount of dust from the Sahara to the Mediterranean. This true-color view from EUMETSAT&#8217;s Meteosat Third Generation (MTG) Flexible Combined Imager (FCI) depicts this situation beautifully. Since MTG-FCI has three visible channels, it is able to produce true color products with fewer assumptions than the GOES-R series of satellites has to rely upon in order to produce similar-looking imagery. This image is from 1230 UTC and is provided courtesy of EUMETSAT&#8217;s <a href=\"https:\/\/view.eumetsat.int\/\">Eumetview<\/a>.  <\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"462\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2026\/03\/wmsMap_2026-03-17T1230-1024x462.png\" alt=\"\" class=\"wp-image-69480\" srcset=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2026\/03\/wmsMap_2026-03-17T1230-1024x462.png 1024w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2026\/03\/wmsMap_2026-03-17T1230-300x135.png 300w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2026\/03\/wmsMap_2026-03-17T1230-768x347.png 768w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2026\/03\/wmsMap_2026-03-17T1230-1536x694.png 1536w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2026\/03\/wmsMap_2026-03-17T1230.png 1920w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/figure>\n\n\n\n<p>Of particular interest is the large dust band that has been pulled from Libya and Egypt into the air over the sea. The <a href=\"https:\/\/rammb.cira.colostate.edu\/training\/visit\/quick_guides\/Dust_RGB_Quick_Guide.pdf\">Dust RGB<\/a> can be used to denote where dust is prevalent. The following image is for the same time. Areas in magenta are associated with dust, and it&#8217;s obvious how widespread the dust is.<\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"462\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2026\/03\/wmsMap_2026-03-17T1230-1-1024x462.png\" alt=\"\" class=\"wp-image-69481\" srcset=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2026\/03\/wmsMap_2026-03-17T1230-1-1024x462.png 1024w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2026\/03\/wmsMap_2026-03-17T1230-1-300x135.png 300w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2026\/03\/wmsMap_2026-03-17T1230-1-768x347.png 768w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2026\/03\/wmsMap_2026-03-17T1230-1-1536x694.png 1536w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2026\/03\/wmsMap_2026-03-17T1230-1.png 1920w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/figure>\n\n\n\n<p>An interesting question is: what kind of storm is this, exactly? A medicane (a portmanteau of &#8220;Mediterranean&#8221; and &#8220;Hurricane&#8221;) is a certain type of cyclone that exhibits some characteristics of a tropical storm, including a warm core and an eye, that separates it from a more traditional mid-latitude cyclone. These are able to use the relatively warm waters of the Mediterranean to develop like a traditional tropical system would, but generally at a much lower intensity. It is March, of course, so the sea surface temperatures are still cool. The 15-16 C temperatures are on the low end of what has been observed with medicanes, but is still possible as much of the dynamical driving is done by upper-level cold air. The ASCAT Winds show a maximum wind speed approaching 40 knots, though it is not clear if the center of the storm is truly calm or if there&#8217;s just an observational gap there.<\/p>\n\n\n\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"740\" height=\"650\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2026\/03\/WMBds158-1.png\" alt=\"\" class=\"wp-image-69484\" srcset=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2026\/03\/WMBds158-1.png 740w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2026\/03\/WMBds158-1-300x264.png 300w\" sizes=\"auto, (max-width: 740px) 100vw, 740px\" \/><\/figure>\n\n\n\n<p>Looking at the animation, there is definitely an eye-like structure at the center of the storm, which is not seen in a standard midlatitude cyclone due to the low-level convergence of those systems.<\/p>\n\n\n\n<figure class=\"wp-block-video\"><video height=\"1018\" style=\"aspect-ratio: 1920 \/ 1018;\" width=\"1920\" controls src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2026\/03\/wmsAnimation_2026-03-17_14_30-2026-03-17_16_30.mp4\"><\/video><\/figure>\n\n\n\n<p>The 700 hPa temperature field from the <a href=\"https:\/\/charts.ecmwf.int\/\">ECMWF model<\/a> from 1200 UTC on the 17th also seems to indicate a hint of a warm core to the system, as can be seen in the bottom center of the graphic below.<\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"922\" src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2026\/03\/20260317195255-85a3da8091c2bfe785f5dee31effb2180aef5063-1024x922.png\" alt=\"\" class=\"wp-image-69482\" srcset=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2026\/03\/20260317195255-85a3da8091c2bfe785f5dee31effb2180aef5063-1024x922.png 1024w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2026\/03\/20260317195255-85a3da8091c2bfe785f5dee31effb2180aef5063-300x270.png 300w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2026\/03\/20260317195255-85a3da8091c2bfe785f5dee31effb2180aef5063-768x691.png 768w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2026\/03\/20260317195255-85a3da8091c2bfe785f5dee31effb2180aef5063-1536x1382.png 1536w, https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2026\/03\/20260317195255-85a3da8091c2bfe785f5dee31effb2180aef5063.png 2000w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/figure>\n\n\n\n<p>Together, these factors have caused some European meteorological centers to officially label this a Medicane. Depending on which agency you listen to, it&#8217;s either called Samuel (France, Andorra) or Jolina (Italy). <\/p>\n","protected":false},"excerpt":{"rendered":"<p>Just north of Libya on the afternoon of 17 March 2026, a large cyclone can be seen forcing a significant amount of dust from the Sahara to the Mediterranean. This true-color view from EUMETSAT&#8217;s Meteosat Third Generation (MTG) Flexible Combined Imager (FCI) depicts this situation beautifully. Since MTG-FCI has three visible channels, it is able [&hellip;]<\/p>\n","protected":false},"author":22,"featured_media":69480,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[7,10,23,25],"tags":[],"class_list":["post-69479","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-air-quality","category-general-interpretation","category-meteosat","category-satellite-winds"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/69479","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\/22"}],"replies":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/comments?post=69479"}],"version-history":[{"count":3,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/69479\/revisions"}],"predecessor-version":[{"id":69488,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/69479\/revisions\/69488"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/69480"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=69479"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=69479"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=69479"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}