{"id":1338,"date":"2023-02-28T11:25:00","date_gmt":"2023-02-28T09:25:00","guid":{"rendered":"https:\/\/projekti.pmfst.unist.hr\/SHExtreme\/?p=1338"},"modified":"2023-09-29T11:49:01","modified_gmt":"2023-09-29T09:49:01","slug":"new-paper-published-3","status":"publish","type":"post","link":"https:\/\/projekti.pmfst.unist.hr\/SHExtreme\/new-paper-published-3\/","title":{"rendered":"Paper on the Adriatic sea level extremes published!"},"content":{"rendered":"\t\t
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Kre\u0161imir Rui\u0107, our PhD student, published a paper on the contribution of high-frequency sea level oscillations to the Adriatic sea level extremes.\u00a0<\/p>

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Sea level time series of up to 17.5 years length, recorded with a 1 min sampling interval at 18 tide gauges, evenly distributed along the eastern and western coast of the Adriatic Sea (Mediterranean), were analysed in order to quantify contribution of high-frequency sea level oscillations to the positive sea level extremes of the Adriatic Sea. Two types of sea level extremes were defined and identified: (1) residual extremes which are mostly related to storm surges and (2) high-frequency (T\u2009<\u20092 h) extremes, strongest of which are meteotsunamis. The detailed analysis of extremes led to the following conclusions: (1) high-frequency sea level oscillations can dominate positive sea level extremes; (2) even when not dominating them, high-frequency oscillations can considerably contribute to extreme sea levels; (3) contribution of high-frequency oscillations to total signal is governed by a combination of bathymetry and atmospheric forcing, resulting in the strongest high-frequency oscillations over the middle Adriatic; (4) residual extremes mostly happen from October to January when they are also the strongest, while high-frequency extremes spread more evenly throughout the year, with the strongest events peaking during May to September; (5) tide gauge stations can be divided into three distinct groups depending on the characteristics of high-frequency oscillations which they record. Conclusively, both low-frequency and high-frequency sea level components must be considered when assessing hazards related to sea level extremes, implying that availability and analysis of 1 min sea level data are a must.<\/p>

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Rui\u0107, K., \u0160epi\u0107, J., Mlinar, M., Me\u0111ugorac, I., 2023. Contribution of high-frequency (T < 2 h) sea level oscillations to the Adriatic sea level maxima. Natural Hazards, 116, 3747-3777. Doi: https:\/\/doi.org\/10.1007\/s11069-023-05834-0<\/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<\/div>\n\t\t","protected":false},"excerpt":{"rendered":"

Kre\u0161imir Rui\u0107, our PhD student, published a paper on the contribution of high-frequency sea level oscillations to the Adriatic sea level extremes.  Sea level time series of up to 17.5 years length, recorded with a 1 min sampling interval at 18 tide gauges, evenly distributed along the eastern and western coast of the Adriatic Sea… Nastavi \u010ditati Paper on the Adriatic sea level extremes published!<\/span><\/a><\/p>\n","protected":false},"author":1,"featured_media":1341,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[12,18],"tags":[],"class_list":["post-1338","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-news","category-scientific-papers","entry"],"_links":{"self":[{"href":"https:\/\/projekti.pmfst.unist.hr\/SHExtreme\/wp-json\/wp\/v2\/posts\/1338","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/projekti.pmfst.unist.hr\/SHExtreme\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/projekti.pmfst.unist.hr\/SHExtreme\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/projekti.pmfst.unist.hr\/SHExtreme\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/projekti.pmfst.unist.hr\/SHExtreme\/wp-json\/wp\/v2\/comments?post=1338"}],"version-history":[{"count":6,"href":"https:\/\/projekti.pmfst.unist.hr\/SHExtreme\/wp-json\/wp\/v2\/posts\/1338\/revisions"}],"predecessor-version":[{"id":1366,"href":"https:\/\/projekti.pmfst.unist.hr\/SHExtreme\/wp-json\/wp\/v2\/posts\/1338\/revisions\/1366"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/projekti.pmfst.unist.hr\/SHExtreme\/wp-json\/wp\/v2\/media\/1341"}],"wp:attachment":[{"href":"https:\/\/projekti.pmfst.unist.hr\/SHExtreme\/wp-json\/wp\/v2\/media?parent=1338"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/projekti.pmfst.unist.hr\/SHExtreme\/wp-json\/wp\/v2\/categories?post=1338"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/projekti.pmfst.unist.hr\/SHExtreme\/wp-json\/wp\/v2\/tags?post=1338"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}