Contribution of high-frequency (T < 2 h) sea level oscillations to the Adriatic sea level maxima
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 pos...
Gespeichert in:
| Veröffentlicht in: | Natural hazards (Dordrecht) 2023-04, Vol.116 (3), p.3747-3777 |
|---|---|
| Hauptverfasser: | , , , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 3777 |
|---|---|
| container_issue | 3 |
| container_start_page | 3747 |
| container_title | Natural hazards (Dordrecht) |
| container_volume | 116 |
| creator | Ruić, Krešimir Šepić, Jadranka Mlinar, Marko Međugorac, Iva |
| description | 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
|
| doi_str_mv | 10.1007/s11069-023-05834-0 |
| format | Article |
| fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_2802189101</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>2802189101</sourcerecordid><originalsourceid>FETCH-LOGICAL-c314t-e95a5a1a144155786bb4bcf5b663c64578297a3c1aeeb0c2129906984017516b3</originalsourceid><addsrcrecordid>eNp9UE1LAzEQDaJgrf4BTwEveojOJJvdDXgpxS8oeFHwFrIx292y3a3JVuzNq__C3-JP8ZeYWkFPHoZhHu_NzHuEHCKcIkB2FhAhVQy4YCBzkTDYIgOUWRzzBLbJABRHBgIedsleCDMAxJSrAXHjru19XSz7umtpV9Kqnlas9O5p6Vq7osd3n69v57H4x3t1QoMztHHPrqFdsHXTmLUs0L6jfeXo6NHXEbF_aHPzUs_NPtkpTRPcwU8fkvvLi7vxNZvcXt2MRxNmBSY9c0oaadBgkqCUWZ4WRVLYUhZpKmyaRISrzAiLxrkCLEeuVLQdHWImMS3EkBxt9i58Fw2EXs-6pW_jSc1z4JgrBIwsvmFZ34XgXakXPj7pVxpBr-PUmzh1jFN_x6khisRGFCK5nTr_u_of1Reys3kr</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2802189101</pqid></control><display><type>article</type><title>Contribution of high-frequency (T < 2 h) sea level oscillations to the Adriatic sea level maxima</title><source>Springer Nature - Complete Springer Journals</source><creator>Ruić, Krešimir ; Šepić, Jadranka ; Mlinar, Marko ; Međugorac, Iva</creator><creatorcontrib>Ruić, Krešimir ; Šepić, Jadranka ; Mlinar, Marko ; Međugorac, Iva</creatorcontrib><description>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
< 2 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.</description><identifier>ISSN: 0921-030X</identifier><identifier>EISSN: 1573-0840</identifier><identifier>DOI: 10.1007/s11069-023-05834-0</identifier><language>eng</language><publisher>Dordrecht: Springer Netherlands</publisher><subject>Atmospheric forcing ; Bathymetry ; Civil Engineering ; Earth and Environmental Science ; Earth Sciences ; Environmental Management ; Gauges ; Geophysics/Geodesy ; Geotechnical Engineering & Applied Earth Sciences ; Hazard assessment ; Hydrogeology ; Natural Hazards ; Original Paper ; Oscillations ; Sea level ; Sea level oscillations ; Storm surges ; Storms ; Tide gauges</subject><ispartof>Natural hazards (Dordrecht), 2023-04, Vol.116 (3), p.3747-3777</ispartof><rights>The Author(s) 2023</rights><rights>The Author(s) 2023. This work is published under http://creativecommons.org/licenses/by/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-c314t-e95a5a1a144155786bb4bcf5b663c64578297a3c1aeeb0c2129906984017516b3</cites><orcidid>0000-0002-5624-1351 ; 0000-0002-1089-4074 ; 0000-0002-9928-8264 ; 0000-0002-3506-697X</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s11069-023-05834-0$$EPDF$$P50$$Gspringer$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s11069-023-05834-0$$EHTML$$P50$$Gspringer$$Hfree_for_read</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Ruić, Krešimir</creatorcontrib><creatorcontrib>Šepić, Jadranka</creatorcontrib><creatorcontrib>Mlinar, Marko</creatorcontrib><creatorcontrib>Međugorac, Iva</creatorcontrib><title>Contribution of high-frequency (T < 2 h) sea level oscillations to the Adriatic sea level maxima</title><title>Natural hazards (Dordrecht)</title><addtitle>Nat Hazards</addtitle><description>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
< 2 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.</description><subject>Atmospheric forcing</subject><subject>Bathymetry</subject><subject>Civil Engineering</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Environmental Management</subject><subject>Gauges</subject><subject>Geophysics/Geodesy</subject><subject>Geotechnical Engineering & Applied Earth Sciences</subject><subject>Hazard assessment</subject><subject>Hydrogeology</subject><subject>Natural Hazards</subject><subject>Original Paper</subject><subject>Oscillations</subject><subject>Sea level</subject><subject>Sea level oscillations</subject><subject>Storm surges</subject><subject>Storms</subject><subject>Tide gauges</subject><issn>0921-030X</issn><issn>1573-0840</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2023</creationdate><recordtype>article</recordtype><sourceid>C6C</sourceid><sourceid>BENPR</sourceid><recordid>eNp9UE1LAzEQDaJgrf4BTwEveojOJJvdDXgpxS8oeFHwFrIx292y3a3JVuzNq__C3-JP8ZeYWkFPHoZhHu_NzHuEHCKcIkB2FhAhVQy4YCBzkTDYIgOUWRzzBLbJABRHBgIedsleCDMAxJSrAXHjru19XSz7umtpV9Kqnlas9O5p6Vq7osd3n69v57H4x3t1QoMztHHPrqFdsHXTmLUs0L6jfeXo6NHXEbF_aHPzUs_NPtkpTRPcwU8fkvvLi7vxNZvcXt2MRxNmBSY9c0oaadBgkqCUWZ4WRVLYUhZpKmyaRISrzAiLxrkCLEeuVLQdHWImMS3EkBxt9i58Fw2EXs-6pW_jSc1z4JgrBIwsvmFZ34XgXakXPj7pVxpBr-PUmzh1jFN_x6khisRGFCK5nTr_u_of1Reys3kr</recordid><startdate>20230401</startdate><enddate>20230401</enddate><creator>Ruić, Krešimir</creator><creator>Šepić, Jadranka</creator><creator>Mlinar, Marko</creator><creator>Međugorac, Iva</creator><general>Springer Netherlands</general><general>Springer Nature B.V</general><scope>C6C</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7ST</scope><scope>7TG</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>KR7</scope><scope>L.G</scope><scope>L6V</scope><scope>M2P</scope><scope>M7S</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>SOI</scope><orcidid>https://orcid.org/0000-0002-5624-1351</orcidid><orcidid>https://orcid.org/0000-0002-1089-4074</orcidid><orcidid>https://orcid.org/0000-0002-9928-8264</orcidid><orcidid>https://orcid.org/0000-0002-3506-697X</orcidid></search><sort><creationdate>20230401</creationdate><title>Contribution of high-frequency (T < 2 h) sea level oscillations to the Adriatic sea level maxima</title><author>Ruić, Krešimir ; Šepić, Jadranka ; Mlinar, Marko ; Međugorac, Iva</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c314t-e95a5a1a144155786bb4bcf5b663c64578297a3c1aeeb0c2129906984017516b3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2023</creationdate><topic>Atmospheric forcing</topic><topic>Bathymetry</topic><topic>Civil Engineering</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Environmental Management</topic><topic>Gauges</topic><topic>Geophysics/Geodesy</topic><topic>Geotechnical Engineering & Applied Earth Sciences</topic><topic>Hazard assessment</topic><topic>Hydrogeology</topic><topic>Natural Hazards</topic><topic>Original Paper</topic><topic>Oscillations</topic><topic>Sea level</topic><topic>Sea level oscillations</topic><topic>Storm surges</topic><topic>Storms</topic><topic>Tide gauges</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Ruić, Krešimir</creatorcontrib><creatorcontrib>Šepić, Jadranka</creatorcontrib><creatorcontrib>Mlinar, Marko</creatorcontrib><creatorcontrib>Međugorac, Iva</creatorcontrib><collection>Springer Nature OA Free Journals</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Environment Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Materials Science & Engineering Collection</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Technology Collection</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>ProQuest Engineering Collection</collection><collection>Science Database</collection><collection>Engineering Database</collection><collection>Environmental Science Database</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Engineering Collection</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><collection>Environment Abstracts</collection><jtitle>Natural hazards (Dordrecht)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Ruić, Krešimir</au><au>Šepić, Jadranka</au><au>Mlinar, Marko</au><au>Međugorac, Iva</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Contribution of high-frequency (T < 2 h) sea level oscillations to the Adriatic sea level maxima</atitle><jtitle>Natural hazards (Dordrecht)</jtitle><stitle>Nat Hazards</stitle><date>2023-04-01</date><risdate>2023</risdate><volume>116</volume><issue>3</issue><spage>3747</spage><epage>3777</epage><pages>3747-3777</pages><issn>0921-030X</issn><eissn>1573-0840</eissn><abstract>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
< 2 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.</abstract><cop>Dordrecht</cop><pub>Springer Netherlands</pub><doi>10.1007/s11069-023-05834-0</doi><tpages>31</tpages><orcidid>https://orcid.org/0000-0002-5624-1351</orcidid><orcidid>https://orcid.org/0000-0002-1089-4074</orcidid><orcidid>https://orcid.org/0000-0002-9928-8264</orcidid><orcidid>https://orcid.org/0000-0002-3506-697X</orcidid><oa>free_for_read</oa></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0921-030X |
| ispartof | Natural hazards (Dordrecht), 2023-04, Vol.116 (3), p.3747-3777 |
| issn | 0921-030X 1573-0840 |
| language | eng |
| recordid | cdi_proquest_journals_2802189101 |
| source | Springer Nature - Complete Springer Journals |
| subjects | Atmospheric forcing Bathymetry Civil Engineering Earth and Environmental Science Earth Sciences Environmental Management Gauges Geophysics/Geodesy Geotechnical Engineering & Applied Earth Sciences Hazard assessment Hydrogeology Natural Hazards Original Paper Oscillations Sea level Sea level oscillations Storm surges Storms Tide gauges |
| title | Contribution of high-frequency (T < 2 h) sea level oscillations to the Adriatic sea level maxima |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-29T23%3A09%3A42IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Contribution%20of%20high-frequency%20(T%E2%80%89%3C%E2%80%892%C2%A0h)%20sea%20level%20oscillations%20to%20the%20Adriatic%20sea%20level%20maxima&rft.jtitle=Natural%20hazards%20(Dordrecht)&rft.au=Rui%C4%87,%20Kre%C5%A1imir&rft.date=2023-04-01&rft.volume=116&rft.issue=3&rft.spage=3747&rft.epage=3777&rft.pages=3747-3777&rft.issn=0921-030X&rft.eissn=1573-0840&rft_id=info:doi/10.1007/s11069-023-05834-0&rft_dat=%3Cproquest_cross%3E2802189101%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=2802189101&rft_id=info:pmid/&rfr_iscdi=true |