Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/5339
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dc.contributor.authorallFaggioni, O.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.authorallSoldani, M.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.authorallPiangiamore, G. L.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.authorallFerrante, A.; Consiglio Superiore dei Lavori Pubblici, via Nomentana 2, Roma, 00161, Italyen
dc.contributor.authorallBencivenga, M.; Servizio Mareografico, Istituto Superiore per la Protezione e la Ricerca Ambientale, via Curtatone 3, Roma, 00185, Italyen
dc.contributor.authorallArena, G.; Servizio Mareografico, Istituto Superiore per la Protezione e la Ricerca Ambientale, via Curtatone 3, Roma, 00185, Italyen
dc.contributor.authorallNardone, G.; Servizio Mareografico, Istituto Superiore per la Protezione e la Ricerca Ambientale, via Curtatone 3, Roma, 00185, Italyen
dc.date.accessioned2009-12-15T10:24:55Zen
dc.date.available2009-12-15T10:24:55Zen
dc.date.issued2008-10-07en
dc.identifier.urihttp://hdl.handle.net/2122/5339en
dc.description.abstractTide is a sea level up-down water motion basically depending on three different phenomena: the Earth-Moon-Sun gravitational relationship, the water surface fluid reaction to atmospheric meteorological dynamic action and the Newtonian vertical adjustment of the sea surface due to atmospheric pressure variations. The first tide component (astro-tide) is periodic and well known in all points of the Earth surface; the second one is directly related to the meteorological phenomenon and then it is foreseeable; the Newtonian component, on the contrary, is not readily predictable by a general hydrostatic law, because the factor “J” that represents the Newtonian transfer (from the atmospheric weight to the consequent sea level) is variable in each harbour area. A statistical study and the related numerical data interpretation of the measurements performed in the Ports of Genoa, La Spezia, Marina di Carrara, Livorno, Piombino, Civitavecchia and Ravenna (belonging to the Italian Newtonian Meteotide Network) show port values of Jph (from 1.4-1.6 cm/hPa to > 2 cm/hPa, on the contrary of the off-shore areas where Jph is about 1 cm/hPa). This phenomenon (hydrobarometric tide wave) produces even double values of harbour sea level fluctuations amplitude in comparison to astronomic tide sea level oscillations, and is characterized by a wavelength from 8-12 h to same days and a 10-25 days/year as mean temporal occurrence in the Northern Tyrrhenian Sea. This is the most relevant ordinary risk factor for our ports activity and structures design. The present note shows a quantitative method to define the values of Jph factor for ports and its use in the Harbour WaterSide Management (HWSM) based on the joined use of barometers, hydrometers and clocks, the preliminary results related to the use of the gravimeters as hydrobarometric predictor in La Spezia Port and two examples of use of Jph factor in the port management: refloating of a landing ship and optimisation of a dock performance as pleasure boats mooring.en
dc.language.isoEnglishen
dc.publisher.namePIANCen
dc.relation.ispartofProceedings of Mediterranean Days of Coastal and Port Engineeringen
dc.subjectmonitoraggio ambientaleen
dc.subjectmareografiaen
dc.subjectmonitoraggio portualeen
dc.titleHarbour water managment for port structures and sea bottom design, coast proximity navigation managment, water quality control.en
dc.typeConference paperen
dc.description.statusPublisheden
dc.subject.INGV03. Hydrosphere::03.01. General::03.01.02. Equatorial and regional oceanographyen
dc.subject.INGV03. Hydrosphere::03.01. General::03.01.04. Ocean data assimilation and reanalysisen
dc.subject.INGV03. Hydrosphere::03.01. General::03.01.08. Instruments and techniquesen
dc.subject.INGV04. Solid Earth::04.03. Geodesy::04.03.05. Gravity variationsen
dc.subject.INGV04. Solid Earth::04.03. Geodesy::04.03.06. Measurements and monitoringen
dc.description.ConferenceLocationPalermo, Italyen
dc.relation.referencesAllen, J.S., D.W. Denbo, 1984. Statistical characteristics of the large-scale response of coastal sea level to atmospheric forcing. J. Phys. Oceanogr. 14:1079-1094. Crépon, M., 1965. Influence de la pression atmosphérique sur le niveau moyen de la Méditerranée Occidentale et sur le flux à travers le Détroit de Gibraltar. Cahiers Océanographiques 17:15-32. El-Gindy, A.A., F.M. Eid, 1990. Long- term variations of monthly mean sea level and its relation to atmospheric pressure in the Mediterranean Sea. Int. Hydrogr. Rev. 17(1):147-159. Faggioni, O., G. Arena, M. Bencivenga, G. Bianco, R. Bozzano, G. Canepa, P. Lusiani, G. Nardone, G.L. Piangiamore, M. Soldani, L. Surace, G. Venzano, 2006. The Newtonian approach in meteorological tide waves forecasting: preliminary observations in the East Ligurian harbours. Annals of Geophysics 49(6):1177-1187. Garrett, C., F. Majaess, 1984. Non-isostatic response of sea-level to atmospheric pressure in the Eastern Mediterranean. J. Phys. Oceanogr. 14:656-665. Garrett, C., B. Toulany, 1982. Sea level variability due to meteorological forcing in the Northeast Gulf of St. Lawrence. J. Geophys. Res. 87(C3):1968–1978. Le Traon, P.-Y., P. Gauzelin, 1997. Response of the Mediterranean mean sea level to atmospheric pressure forcing, J. Geophys. Res. 102(C1):973–984. Mosetti, F., 1969. Oscillazioni del livello medio marino a Venezia in rapporto con le oscillazioni di pressione atmosferica. Boll. Geof. Teor. ed Appl. 11(43-44):264-277. Stocchino, C., V. Scotto, 1970. Il livello marino e la pressione atmosferica nel porto di Genova. Bull. Inst. Océanogr. Monaco 69(1399):1-10. Tsimplis, M.N. 1995. The response of sea level to atmospheric forcing in the Mediterranean. J. Coastal Res. 11(4):1309-1321. Tsimplis, M.N., G.N. Vlahakis, 1994. Meteorological forcing and sea level variability in the Aegean Sea. J. Geophys. Res. 99(C5):9879-9890.en
dc.description.obiettivoSpecifico1.8. Osservazioni di geofisica ambientaleen
dc.description.obiettivoSpecifico3.7. Dinamica del clima e dell'oceanoen
dc.description.obiettivoSpecifico3.8. Geofisica per l'ambienteen
dc.description.fulltextopenen
dc.contributor.authorFaggioni, O.en
dc.contributor.authorSoldani, M.en
dc.contributor.authorPiangiamore, G. L.en
dc.contributor.authorFerrante, A.en
dc.contributor.authorBencivenga, M.en
dc.contributor.authorArena, G.en
dc.contributor.authorNardone, G.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.departmentConsiglio Superiore dei Lavori Pubblici, via Nomentana 2, Roma, 00161, Italyen
dc.contributor.departmentServizio Mareografico, Istituto Superiore per la Protezione e la Ricerca Ambientale, via Curtatone 3, Roma, 00185, Italyen
dc.contributor.departmentServizio Mareografico, Istituto Superiore per la Protezione e la Ricerca Ambientale, via Curtatone 3, Roma, 00185, Italyen
dc.contributor.departmentServizio Mareografico, Istituto Superiore per la Protezione e la Ricerca Ambientale, via Curtatone 3, Roma, 00185, Italyen
item.openairetypeConference paper-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia-
crisitem.author.deptConsiglio Superiore dei Lavori Pubblici, via Nomentana 2, Roma, 00161, Italy-
crisitem.author.deptIstituto Superiore per la Protezione e la Ricerca Ambientale-
crisitem.author.deptServizio Mareografico, Istituto Superiore per la Protezione e la Ricerca Ambientale, via Curtatone 3, Roma, 00185, Italy-
crisitem.author.orcid0000-0002-9772-3453-
crisitem.author.orcid0000-0001-7039-2781-
crisitem.author.orcid0000-0002-8776-7954-
crisitem.author.orcid0000-0002-2724-4879-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent03. Hydrosphere-
crisitem.classification.parent03. Hydrosphere-
crisitem.classification.parent03. Hydrosphere-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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