Contribution of high-frequency (T < 2 h) sea level oscillations to the Adriatic sea level maxima
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 t...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Ruić, Krešimir [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2023 |
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| Schlagwörter: |
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| Anmerkung: |
© The Author(s) 2023 |
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| Übergeordnetes Werk: |
Enthalten in: Natural hazards - Dordrecht [u.a.] : Springer Science + Business Media B.V., 1988, 116(2023), 3 vom: 15. Feb., Seite 3747-3777 |
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| Übergeordnetes Werk: |
volume:116 ; year:2023 ; number:3 ; day:15 ; month:02 ; pages:3747-3777 |
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| DOI / URN: |
10.1007/s11069-023-05834-0 |
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| 100 | 1 | |a Ruić, Krešimir |e verfasserin |0 (orcid)0000-0002-3506-697X |4 aut | |
| 245 | 1 | 0 | |a Contribution of high-frequency (T < 2 h) sea level oscillations to the Adriatic sea level maxima |
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| 520 | |a 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. | ||
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| 650 | 4 | |a High-frequency sea level oscillations |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Meteotsunamis |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Storm surges |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Adriatic Sea |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Šepić, Jadranka |0 (orcid)0000-0002-5624-1351 |4 aut | |
| 700 | 1 | |a Mlinar, Marko |0 (orcid)0000-0002-1089-4074 |4 aut | |
| 700 | 1 | |a Međugorac, Iva |0 (orcid)0000-0002-9928-8264 |4 aut | |
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10.1007/s11069-023-05834-0 doi (DE-627)SPR050066250 (SPR)s11069-023-05834-0-e DE-627 ger DE-627 rakwb eng Ruić, Krešimir verfasserin (orcid)0000-0002-3506-697X aut Contribution of high-frequency (T < 2 h) sea level oscillations to the Adriatic sea level maxima 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) 2023 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. Sea level (dpeaa)DE-He213 High-frequency sea level oscillations (dpeaa)DE-He213 Meteotsunamis (dpeaa)DE-He213 Storm surges (dpeaa)DE-He213 Adriatic Sea (dpeaa)DE-He213 Šepić, Jadranka (orcid)0000-0002-5624-1351 aut Mlinar, Marko (orcid)0000-0002-1089-4074 aut Međugorac, Iva (orcid)0000-0002-9928-8264 aut Enthalten in Natural hazards Dordrecht [u.a.] : Springer Science + Business Media B.V., 1988 116(2023), 3 vom: 15. Feb., Seite 3747-3777 (DE-627)315621729 (DE-600)2017806-2 1573-0840 nnns volume:116 year:2023 number:3 day:15 month:02 pages:3747-3777 https://dx.doi.org/10.1007/s11069-023-05834-0 kostenfrei Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 116 2023 3 15 02 3747-3777 |
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10.1007/s11069-023-05834-0 doi (DE-627)SPR050066250 (SPR)s11069-023-05834-0-e DE-627 ger DE-627 rakwb eng Ruić, Krešimir verfasserin (orcid)0000-0002-3506-697X aut Contribution of high-frequency (T < 2 h) sea level oscillations to the Adriatic sea level maxima 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) 2023 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. Sea level (dpeaa)DE-He213 High-frequency sea level oscillations (dpeaa)DE-He213 Meteotsunamis (dpeaa)DE-He213 Storm surges (dpeaa)DE-He213 Adriatic Sea (dpeaa)DE-He213 Šepić, Jadranka (orcid)0000-0002-5624-1351 aut Mlinar, Marko (orcid)0000-0002-1089-4074 aut Međugorac, Iva (orcid)0000-0002-9928-8264 aut Enthalten in Natural hazards Dordrecht [u.a.] : Springer Science + Business Media B.V., 1988 116(2023), 3 vom: 15. Feb., Seite 3747-3777 (DE-627)315621729 (DE-600)2017806-2 1573-0840 nnns volume:116 year:2023 number:3 day:15 month:02 pages:3747-3777 https://dx.doi.org/10.1007/s11069-023-05834-0 kostenfrei Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 116 2023 3 15 02 3747-3777 |
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10.1007/s11069-023-05834-0 doi (DE-627)SPR050066250 (SPR)s11069-023-05834-0-e DE-627 ger DE-627 rakwb eng Ruić, Krešimir verfasserin (orcid)0000-0002-3506-697X aut Contribution of high-frequency (T < 2 h) sea level oscillations to the Adriatic sea level maxima 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) 2023 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. Sea level (dpeaa)DE-He213 High-frequency sea level oscillations (dpeaa)DE-He213 Meteotsunamis (dpeaa)DE-He213 Storm surges (dpeaa)DE-He213 Adriatic Sea (dpeaa)DE-He213 Šepić, Jadranka (orcid)0000-0002-5624-1351 aut Mlinar, Marko (orcid)0000-0002-1089-4074 aut Međugorac, Iva (orcid)0000-0002-9928-8264 aut Enthalten in Natural hazards Dordrecht [u.a.] : Springer Science + Business Media B.V., 1988 116(2023), 3 vom: 15. Feb., Seite 3747-3777 (DE-627)315621729 (DE-600)2017806-2 1573-0840 nnns volume:116 year:2023 number:3 day:15 month:02 pages:3747-3777 https://dx.doi.org/10.1007/s11069-023-05834-0 kostenfrei Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 116 2023 3 15 02 3747-3777 |
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10.1007/s11069-023-05834-0 doi (DE-627)SPR050066250 (SPR)s11069-023-05834-0-e DE-627 ger DE-627 rakwb eng Ruić, Krešimir verfasserin (orcid)0000-0002-3506-697X aut Contribution of high-frequency (T < 2 h) sea level oscillations to the Adriatic sea level maxima 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) 2023 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. Sea level (dpeaa)DE-He213 High-frequency sea level oscillations (dpeaa)DE-He213 Meteotsunamis (dpeaa)DE-He213 Storm surges (dpeaa)DE-He213 Adriatic Sea (dpeaa)DE-He213 Šepić, Jadranka (orcid)0000-0002-5624-1351 aut Mlinar, Marko (orcid)0000-0002-1089-4074 aut Međugorac, Iva (orcid)0000-0002-9928-8264 aut Enthalten in Natural hazards Dordrecht [u.a.] : Springer Science + Business Media B.V., 1988 116(2023), 3 vom: 15. Feb., Seite 3747-3777 (DE-627)315621729 (DE-600)2017806-2 1573-0840 nnns volume:116 year:2023 number:3 day:15 month:02 pages:3747-3777 https://dx.doi.org/10.1007/s11069-023-05834-0 kostenfrei Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 116 2023 3 15 02 3747-3777 |
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10.1007/s11069-023-05834-0 doi (DE-627)SPR050066250 (SPR)s11069-023-05834-0-e DE-627 ger DE-627 rakwb eng Ruić, Krešimir verfasserin (orcid)0000-0002-3506-697X aut Contribution of high-frequency (T < 2 h) sea level oscillations to the Adriatic sea level maxima 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) 2023 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. Sea level (dpeaa)DE-He213 High-frequency sea level oscillations (dpeaa)DE-He213 Meteotsunamis (dpeaa)DE-He213 Storm surges (dpeaa)DE-He213 Adriatic Sea (dpeaa)DE-He213 Šepić, Jadranka (orcid)0000-0002-5624-1351 aut Mlinar, Marko (orcid)0000-0002-1089-4074 aut Međugorac, Iva (orcid)0000-0002-9928-8264 aut Enthalten in Natural hazards Dordrecht [u.a.] : Springer Science + Business Media B.V., 1988 116(2023), 3 vom: 15. Feb., Seite 3747-3777 (DE-627)315621729 (DE-600)2017806-2 1573-0840 nnns volume:116 year:2023 number:3 day:15 month:02 pages:3747-3777 https://dx.doi.org/10.1007/s11069-023-05834-0 kostenfrei Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 116 2023 3 15 02 3747-3777 |
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Enthalten in Natural hazards 116(2023), 3 vom: 15. Feb., Seite 3747-3777 volume:116 year:2023 number:3 day:15 month:02 pages:3747-3777 |
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Ruić, Krešimir @@aut@@ Šepić, Jadranka @@aut@@ Mlinar, Marko @@aut@@ Međugorac, Iva @@aut@@ |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000naa a22002652 4500</leader><controlfield tag="001">SPR050066250</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230418064729.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">230418s2023 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s11069-023-05834-0</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR050066250</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)s11069-023-05834-0-e</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Ruić, Krešimir</subfield><subfield code="e">verfasserin</subfield><subfield code="0">(orcid)0000-0002-3506-697X</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Contribution of high-frequency (T < 2 h) sea level oscillations to the Adriatic sea level maxima</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2023</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© The Author(s) 2023</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">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.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Sea level</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">High-frequency sea level oscillations</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Meteotsunamis</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Storm surges</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Adriatic Sea</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Šepić, Jadranka</subfield><subfield code="0">(orcid)0000-0002-5624-1351</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Mlinar, Marko</subfield><subfield code="0">(orcid)0000-0002-1089-4074</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Međugorac, Iva</subfield><subfield code="0">(orcid)0000-0002-9928-8264</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Natural hazards</subfield><subfield code="d">Dordrecht [u.a.] : Springer Science + Business Media B.V., 1988</subfield><subfield code="g">116(2023), 3 vom: 15. 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Ruić, Krešimir |
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Ruić, Krešimir misc Sea level misc High-frequency sea level oscillations misc Meteotsunamis misc Storm surges misc Adriatic Sea Contribution of high-frequency (T < 2 h) sea level oscillations to the Adriatic sea level maxima |
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Contribution of high-frequency (T < 2 h) sea level oscillations to the Adriatic sea level maxima Sea level (dpeaa)DE-He213 High-frequency sea level oscillations (dpeaa)DE-He213 Meteotsunamis (dpeaa)DE-He213 Storm surges (dpeaa)DE-He213 Adriatic Sea (dpeaa)DE-He213 |
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Contribution of high-frequency (T < 2 h) sea level oscillations to the Adriatic sea level maxima |
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Contribution of high-frequency (T < 2 h) sea level oscillations to the Adriatic sea level maxima |
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contribution of high-frequency (t < 2 h) sea level oscillations to the adriatic sea level maxima |
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Contribution of high-frequency (T < 2 h) sea level oscillations to the Adriatic sea level maxima |
| abstract |
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. © The Author(s) 2023 |
| abstractGer |
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. © The Author(s) 2023 |
| abstract_unstemmed |
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. © The Author(s) 2023 |
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Contribution of high-frequency (T < 2 h) sea level oscillations to the Adriatic sea level maxima |
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https://dx.doi.org/10.1007/s11069-023-05834-0 |
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Šepić, Jadranka Mlinar, Marko Međugorac, Iva |
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Šepić, Jadranka Mlinar, Marko Međugorac, Iva |
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10.1007/s11069-023-05834-0 |
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2024-07-04T03:19:09.354Z |
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| score |
7.398978 |