{"id":1670,"date":"2020-05-17T18:57:00","date_gmt":"2020-05-17T16:57:00","guid":{"rendered":"https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/?p=1670"},"modified":"2023-12-20T09:29:30","modified_gmt":"2023-12-20T07:29:30","slug":"33-vrboska-hvar-island-vela-luka-korcula-island-14-16-may-2020","status":"publish","type":"post","link":"https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/33-vrboska-hvar-island-vela-luka-korcula-island-14-16-may-2020\/","title":{"rendered":"(33) Vrboska,  Vela Luka,  14-16 May 2020"},"content":{"rendered":"\t\t<div data-elementor-type=\"wp-post\" data-elementor-id=\"1670\" class=\"elementor elementor-1670\" data-elementor-post-type=\"post\">\n\t\t\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-18a90dd3 elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"18a90dd3\" 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-6bfc0721\" data-id=\"6bfc0721\" 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-75ca782e elementor-widget elementor-widget-heading\" data-id=\"75ca782e\" 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\">(33) Vela Luka, Vrboska, 14-16 May 2020<\/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-302c2d89 elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"302c2d89\" 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-77a40fd1\" data-id=\"77a40fd1\" 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-221fcea elementor-widget elementor-widget-image\" data-id=\"221fcea\" 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_14_May_2020-scaled.jpg\" class=\"attachment-full size-full wp-image-2378\" alt=\"\" srcset=\"https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-content\/uploads\/2023\/03\/synoptic_events_14_May_2020-scaled.jpg 2560w, https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-content\/uploads\/2023\/03\/synoptic_events_14_May_2020-300x97.jpg 300w, https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-content\/uploads\/2023\/03\/synoptic_events_14_May_2020-1024x331.jpg 1024w, https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-content\/uploads\/2023\/03\/synoptic_events_14_May_2020-768x248.jpg 768w, https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-content\/uploads\/2023\/03\/synoptic_events_14_May_2020-1536x497.jpg 1536w, https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-content\/uploads\/2023\/03\/synoptic_events_14_May_2020-2048x662.jpg 2048w, https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-content\/uploads\/2023\/03\/synoptic_events_14_May_2020-1568x507.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-36636a6c elementor-widget elementor-widget-text-editor\" data-id=\"36636a6c\" 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>Only three days after the previous event, during 14-15 May 2020, meteotsunamis again occurred at Vrboska and Vela Luka. Descriptive information on Vrboska event come from on-line articles and YouTube (<a href=\"https:\/\/www.youtube.com\/watch?v=-aD9q4QMANE\" target=\"_blank\" rel=\"noopener\">YouTube, 15 May 2020<\/a>). According to these, strong sea-level oscillations were observed during early afternoon hours of 14 May. The oscillations had 5-6 min period and resulted in drying and 30-cm flooding of the bay. In Vela Luka, sea-level oscillations caused drying and flooding of the inner bay as well. Vela Luka tide-gauge measurements reveal that high-frequency sea-level oscillations were strongest between 10:00 and 16:00 UTC of 14 May, and then again between 21:00 UTC of 15 May and 02:00 UTC of 16 May. On 14 May, maximum wave of 71.0 cm height was recorded between 14:48 and 15:02 UTC, and average period of dominant oscillations was 12-13 min. On 15 May, maximum wave of 80.3 cm was recorded between 22:50 and 23:03 UTC, and average period of dominant oscillations was 16-18 min. In spite of fact that sea-level oscillations were equal or even somewhat stronger than those observed three days earlier, air pressure data from both Vrboska and Vela Luka reveal much weaker air pressure disturbances reaching maximum heights of 1.4 hPa (both locations), and maximum 5-min rates of air pressure oscillations of -0.7 hPa\/5 min (Vrboska), i.e. -1.1 hPa\/5 min (Vela Luka). Nonetheless, the high-frequency air pressure oscillations were present through a better part of 14-15 May 2020. Both atmospheric and ocean component of the event were numerically modelled by\u00a0<a href=\"https:\/\/nhess.copernicus.org\/articles\/21\/2427\/2021\/\" target=\"_blank\" rel=\"noopener\">Toj\u010di\u0107 et al. (2021)<\/a>\u00a0with the meteotsunami module of real-time one-way coupled atmosphere-ocean AdriSC model.\u00a0<\/p><p>\u00a0<\/p><p>\u00a0<\/p><p>Synoptic situation slightly differed from the situation during the\u00a0<a href=\"https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/32-vrboska-hvar-island-vela-luka-korcula-island-11-may-2020\/\" target=\"_blank\" rel=\"noopener\">Event 32<\/a>\u00a0which occurred three days earlier.\u00a0<span style=\"font-family: Montserrat; font-size: 13.5pt; color: var( --e-global-color-text );\">Synoptic situation over Europe was now\u00a0<\/span><span style=\"font-family: Montserrat; font-size: 13.5pt; color: var( --e-global-color-text );\">dominated by a low off the Portuguese coast\u00a0 with related weak mean sea level\u00a0<\/span><span style=\"font-family: Montserrat; font-size: 13.5pt; color: var( --e-global-color-text );\">pressure gradients over the Mediterranean and the Adriatic Sea. Over\u00a0<\/span><span style=\"font-family: Montserrat; font-size: 13.5pt; color: var( --e-global-color-text );\">the Adriatic Sea weak sirocco was blowing, reaching speeds from 10 to 16 m\/s.\u00a0<\/span><span style=\"font-size: 13.5pt; background-image: initial; background-position: initial; background-size: initial; background-repeat: initial; background-attachment: initial; background-origin: initial; background-clip: initial; line-height: 19.26px; font-family: Montserrat; color: black;\"><span style=\"color: var( --e-global-color-text );\">At the 850 hPa, a warm air mass was advancing from the\u00a0<\/span><\/span><span style=\"color: var( --e-global-color-text ); font-family: Montserrat; font-size: 13.5pt;\">central Sahara, across the central Mediterranean towards the Adriatic Sea. As a\u00a0<\/span><span style=\"color: var( --e-global-color-text ); font-family: Montserrat; font-size: 13.5pt;\">result, an upper-level temperature front was still well developed over the Adriatic Sea. At\u00a0<\/span><span style=\"color: var( --e-global-color-text ); font-family: Montserrat; font-size: 13.5pt;\">the 500 hPa height, strong south-westerly winds (up to 38 m\/s), related to a deep low, blew over\u00a0<\/span><span style=\"color: var( --e-global-color-text ); font-size: 13.5pt; font-family: Montserrat;\">the Adriatic.<\/span><span style=\"color: var( --e-global-color-text ); font-size: 13.5pt; font-family: Montserrat;\">\u00a0<\/span><span style=\"color: var( --e-global-color-text ); font-size: 0.9em;\">\u00a0<\/span><\/p><p>\u00a0<\/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-790e7968 elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"790e7968\" 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-601fca79\" data-id=\"601fca79\" 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-48dd84a6 elementor-widget elementor-widget-image\" data-id=\"48dd84a6\" 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=\"1379\" height=\"1860\" src=\"https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-content\/uploads\/2022\/03\/33-Vrboska-Hvar-Island-Vela-Luka-Korcula-Island-2.jpg\" class=\"attachment-full size-full wp-image-1676\" alt=\"(33) Vrboska, Hvar Island; Vela Luka, Kor\u010dula Island\" srcset=\"https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-content\/uploads\/2022\/03\/33-Vrboska-Hvar-Island-Vela-Luka-Korcula-Island-2.jpg 1379w, https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-content\/uploads\/2022\/03\/33-Vrboska-Hvar-Island-Vela-Luka-Korcula-Island-2-222x300.jpg 222w, https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-content\/uploads\/2022\/03\/33-Vrboska-Hvar-Island-Vela-Luka-Korcula-Island-2-759x1024.jpg 759w, https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-content\/uploads\/2022\/03\/33-Vrboska-Hvar-Island-Vela-Luka-Korcula-Island-2-768x1036.jpg 768w, https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-content\/uploads\/2022\/03\/33-Vrboska-Hvar-Island-Vela-Luka-Korcula-Island-2-1139x1536.jpg 1139w\" sizes=\"(max-width: 1379px) 100vw, 1379px\" style=\"width:100%;height:134.88%;max-width:1379px\" \/>\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 Vela Luka, and high-pass filtered (T &lt; 4 h) air pressure time series measured at Vela Luka and Vrboska, all during Events 32 and 33. <\/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>(33) Vela Luka, Vrboska, 14-16 May 2020 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. Only three days after the previous event, during 14-15 May 2020, meteotsunamis again occurred at&hellip; <a class=\"more-link\" href=\"https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/33-vrboska-hvar-island-vela-luka-korcula-island-14-16-may-2020\/\">Continue reading <span class=\"screen-reader-text\">(33) Vrboska,  Vela Luka,  14-16 May 2020<\/span><\/a><\/p>\n","protected":false},"author":1,"featured_media":2378,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[23],"tags":[],"class_list":["post-1670","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\/1670","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=1670"}],"version-history":[{"count":29,"href":"https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-json\/wp\/v2\/posts\/1670\/revisions"}],"predecessor-version":[{"id":3566,"href":"https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-json\/wp\/v2\/posts\/1670\/revisions\/3566"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-json\/wp\/v2\/media\/2378"}],"wp:attachment":[{"href":"https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-json\/wp\/v2\/media?parent=1670"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-json\/wp\/v2\/categories?post=1670"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/projekti.pmfst.unist.hr\/floods\/meteotsunamis\/wp-json\/wp\/v2\/tags?post=1670"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}