{"id":1995,"date":"2017-07-12T15:39:00","date_gmt":"2017-07-12T13:39:00","guid":{"rendered":"https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/?p=1995"},"modified":"2023-05-23T14:12:27","modified_gmt":"2023-05-23T12:12:27","slug":"25-mali-losinj-11-july-2017","status":"publish","type":"post","link":"https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/25-mali-losinj-11-july-2017\/","title":{"rendered":"(25) Mali Lo\u0161inj, 11 July 2017"},"content":{"rendered":"\t\t<div data-elementor-type=\"wp-post\" data-elementor-id=\"1995\" class=\"elementor elementor-1995\" data-elementor-post-type=\"post\">\n\t\t\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-64283aaa elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"64283aaa\" data-element_type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-1c02075d\" data-id=\"1c02075d\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-54df279f elementor-widget elementor-widget-heading\" data-id=\"54df279f\" data-element_type=\"widget\" data-widget_type=\"heading.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<h3 class=\"elementor-heading-title elementor-size-default\">(25) Mali Lo\u0161inj, 11 July 2017<\/h3>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-750eda9a elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"750eda9a\" data-element_type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-5e5acf9f\" data-id=\"5e5acf9f\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-2954359 elementor-widget elementor-widget-image\" data-id=\"2954359\" data-element_type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t\t\t\t<figure class=\"wp-caption\">\n\t\t\t\t\t\t\t\t\t\t<img fetchpriority=\"high\" decoding=\"async\" width=\"2560\" height=\"828\" src=\"https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-content\/uploads\/2023\/03\/synoptic_events_11_Jul_2017-scaled.jpg\" class=\"attachment-full size-full wp-image-2382\" alt=\"\" srcset=\"https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-content\/uploads\/2023\/03\/synoptic_events_11_Jul_2017-scaled.jpg 2560w, https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-content\/uploads\/2023\/03\/synoptic_events_11_Jul_2017-300x97.jpg 300w, https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-content\/uploads\/2023\/03\/synoptic_events_11_Jul_2017-1024x331.jpg 1024w, https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-content\/uploads\/2023\/03\/synoptic_events_11_Jul_2017-768x248.jpg 768w, https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-content\/uploads\/2023\/03\/synoptic_events_11_Jul_2017-1536x497.jpg 1536w, https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-content\/uploads\/2023\/03\/synoptic_events_11_Jul_2017-2048x662.jpg 2048w, https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-content\/uploads\/2023\/03\/synoptic_events_11_Jul_2017-1568x507.jpg 1568w\" sizes=\"(max-width: 2560px) 100vw, 2560px\" style=\"width:100%;height:32.34%;max-width:2560px\" \/>\t\t\t\t\t\t\t\t\t\t\t<figcaption class=\"widget-image-caption wp-caption-text\">Figure 1. Synoptic situation at the time of the event: (left) mean sea level pressure and 10-m wind; (middle) temperature and wind at 850 hPa; (right) geopotential height and wind at 500 hPa.<\/figcaption>\n\t\t\t\t\t\t\t\t\t\t<\/figure>\n\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-ef8ae6f elementor-widget elementor-widget-text-editor\" data-id=\"ef8ae6f\" data-element_type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<p>Several locations on the island of Lo\u0161inj were hit by meteotsunami waves between 18:00 and 19:00 UTC on 11 July 2017. These locations are: (1) bay Krivica, (2) bay \u010cikat, and (3) town of Mali Lo\u0161inj. Event was strongest in bay Krivica where about 20 leisure boats were moored. According to eyewitnesses, sea suddenly retreated from the bay around 18:00 UTC, leaving uppermost 30 m of the bay length completely dry (<a href=\"https:\/\/www.burzanautike.com\/hr\/vecer_kad_se_apoksiomen_pozelio_vratiti_moru\/4660\/57\" target=\"_blank\">Burza nauzike, 27 July 2017<\/a>). As a result, numerous boats were stranded on the dry sea bottom. A few minutes later, a big &#8220;tidal wave&#8221; brought sea back to the bay ejecting some of the boats on the coast. Strong sea currents moved cement mooring blocks from the sea bottom. Altogether, three pronounced waves were observed within a 15-min period, yielding an approximate period of oscillations of ~5 min.<\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-9bb9e50 elementor-widget elementor-widget-text-editor\" data-id=\"9bb9e50\" data-element_type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<p>Waves in the bay of \u010cikat were filmed by a YouTube user jedro43 (<a href=\"https:\/\/www.youtube.com\/watch?v=-iu63d6i_Lc\" target=\"_blank\" rel=\"noopener\">YouTube, 12 July 2017a<\/a>). Although, the event was not as dramatic as in Krivica bay, the video depicting it is very professional and gives us valuable information on the event. During 5:33 min of video, sea advanced and retreated 3 times, yielding an approximate period of oscillations of ~2-3 min. Height of sea level oscillations (detectable from harbor structures and author&#8217;s comments) was ~1 m. Finally, event was also strong in the town of Mali Lo\u0161inj, where sea arose over promenade flooding numerous cafes, shops, and local museum. Flooding of Mali Lo\u0161inj was filmed by a YouTube user Dule 1950 (<a href=\"https:\/\/www.youtube.com\/watch?v=qDGaFSGu_tY\" target=\"_blank\" rel=\"noopener\">YouTube, 12 July 2017b<\/a>). According to eyewitnesses, the event was accompanied by a strong thunderstorm, rain and winds of up to 40 knots.<\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-990a9e5 elementor-widget elementor-widget-text-editor\" data-id=\"990a9e5\" data-element_type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<p>An increase in high-frequency variability was also recorded by the ~80 km distanced Bakar tide gauge. High-frequency sea level oscillations in Bakar were intensified from ~19:00 of 11 July till ~04:00 UCT of the following day. The maximum oscillation with a 51.5 cm crest-to-trough height was recorded around midnight of 12 July.&nbsp;<br><\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-b090bbb elementor-widget elementor-widget-text-editor\" data-id=\"b090bbb\" data-element_type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<p>Atmospheric and sea level component of the event were also numerically modelled using AdriSC modelling suite (using the Weather Research and Forecast model for the atmospheric component and ROMS\/ADCIRC model for the ocean component), by Denamiel et al. (<a style=\"background-color: #ffffff;\" href=\"https:\/\/www.sciencedirect.com\/science\/article\/abs\/pii\/S1463500318302464\" target=\"_blank\" rel=\"noopener\">2019a<\/a>,\u00a0<a style=\"background-color: #ffffff;\" href=\"https:\/\/journals.ametsoc.org\/view\/journals\/phoc\/50\/4\/jpo-d-19-0147.1.xml\" target=\"_blank\" rel=\"noopener\">2020<\/a>).\u00a0<\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-3ce0e17 elementor-widget elementor-widget-text-editor\" data-id=\"3ce0e17\" data-element_type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<p><span style=\"text-align: justify;\">The synoptic situation during the event was characterized by weak pressure gradients over the Mediterranean and most of Europe, and corresponding weak surface winds. At the 850-hPa level, warm air was advancing from the western Sahara across the western Mediterranean towards the Adriatic Sea and the southeastern Europe. Upper-level temperature gradients were present over the Adriatic Sea. At the 500 hPa level westerly mid-tropospheric winds with speeds up to 28 m\/s were blowing over the western Mediterranean and the northern Adriatic.&nbsp;<\/span><\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-46bd6c6 elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"46bd6c6\" data-element_type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-9181f10\" data-id=\"9181f10\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-7e7857b elementor-widget elementor-widget-image\" data-id=\"7e7857b\" data-element_type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t\t\t\t<figure class=\"wp-caption\">\n\t\t\t\t\t\t\t\t\t\t<img decoding=\"async\" width=\"750\" height=\"666\" src=\"https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-content\/uploads\/2017\/07\/ts_no25-1024x909.jpg\" class=\"attachment-large size-large wp-image-2458\" alt=\"\" srcset=\"https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-content\/uploads\/2017\/07\/ts_no25-1024x909.jpg 1024w, https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-content\/uploads\/2017\/07\/ts_no25-300x266.jpg 300w, https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-content\/uploads\/2017\/07\/ts_no25-768x682.jpg 768w, https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-content\/uploads\/2017\/07\/ts_no25-1536x1364.jpg 1536w, https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-content\/uploads\/2017\/07\/ts_no25-1568x1392.jpg 1568w, https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-content\/uploads\/2017\/07\/ts_no25.jpg 2024w\" sizes=\"(max-width: 750px) 100vw, 750px\" style=\"width:100%;height:88.78%;max-width:2024px\" \/>\t\t\t\t\t\t\t\t\t\t\t<figcaption class=\"widget-image-caption wp-caption-text\">Figure 2. Original and high-pass (T &lt; 4h) sea-level time series measured at Bakar during Event 25.<\/figcaption>\n\t\t\t\t\t\t\t\t\t\t<\/figure>\n\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<\/div>\n\t\t","protected":false},"excerpt":{"rendered":"<p>(25) Mali Lo\u0161inj, 11 July 2017 Figure 1. Synoptic situation at the time of the event: (left) mean sea level pressure and 10-m wind; (middle) temperature and wind at 850 hPa; (right) geopotential height and wind at 500 hPa. Several locations on the island of Lo\u0161inj were hit by meteotsunami waves between 18:00 and 19:00&hellip; <a class=\"more-link\" href=\"https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/25-mali-losinj-11-july-2017\/\">Continue reading <span class=\"screen-reader-text\">(25) Mali Lo\u0161inj, 11 July 2017<\/span><\/a><\/p>\n","protected":false},"author":1,"featured_media":2382,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[23],"tags":[],"class_list":["post-1995","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-meteotsunami","entry"],"_links":{"self":[{"href":"https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-json\/wp\/v2\/posts\/1995","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-json\/wp\/v2\/comments?post=1995"}],"version-history":[{"count":37,"href":"https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-json\/wp\/v2\/posts\/1995\/revisions"}],"predecessor-version":[{"id":3445,"href":"https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-json\/wp\/v2\/posts\/1995\/revisions\/3445"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-json\/wp\/v2\/media\/2382"}],"wp:attachment":[{"href":"https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-json\/wp\/v2\/media?parent=1995"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-json\/wp\/v2\/categories?post=1995"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-json\/wp\/v2\/tags?post=1995"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}