Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/6914
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dc.contributor.authorallMarini, M.; Institue of Marine Science, National Research Centeren
dc.contributor.authorallGrilli, F.; Institue of Marine Science, National Research Centeren
dc.contributor.authorallGuarnieri, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italiaen
dc.contributor.authorallBurton, H. J.; University of Southern California, Los Angelesen
dc.contributor.authorallKlajic, Z.; Institute of Marine Biology Kotor, Montenegroen
dc.contributor.authorallPinardi, N.; CIRSA, University of Bologna, Ravenna, Italyen
dc.contributor.authorallSanxhaku, M.; Institute of Hydrometeorology, Tirana, Albaniaen
dc.date.accessioned2011-01-26T10:30:21Zen
dc.date.available2011-01-26T10:30:21Zen
dc.date.issued2010-04-21en
dc.identifier.urihttp://hdl.handle.net/2122/6914en
dc.description.abstractThis study intends to understand and assess the effects of the discharge from the Buna/Bojana river delta watersheds on the eutrophic status of the southeastern Adriatic Sea, and contrast this area with the northwestern Adriatic region where the Po River dominates the freshwater discharge into the coastal ocean. We compare observations of inorganic nutrients, turbidity, and physical variables from the two regions and use numerical model results to characterize the physical circulation of the two areas. The area affected by the Po River discharge extends at least one hundred kilometers southward from the delta and approximately 20 km offshore. Maximum chlorophyll concentrations typically occur within the river plume. Similarly, in the southeastern Adriatic Sea, the Buna/Bojana River discharge extends northward along the coasts for approximately one hundred kilometers and contains a large maxima in the regional chlorophyll distribution. The two coastal areas tend to have opposing physical forcing processes: the Po River tends to be affected area by northerly to northeasterly winds that cause downwelling, whereas the Buna/Bojana River on the opposite side of the basin is typically characterized by northerly, upwelling favorable winds. However, during the study period, upwelling is not a dominant feature of the circulation and both the shelf slope current (SouthEastern Adriatic e SEAd current) and the along shore currents in the southeastern Adriatic Sea are northward. The along shore current probably dominated by the river runoff is here described for the first time and called the southeastern Shelf Coastal (SESC) current. Under these conditions, primary productivity is high in both regions leading us to conclude that river plume dynamics and the associated nutrient inputs determine the eutrophication status of the coastal strip, regardless of the circulation regime in the southeastern Adriatic Sea area. The Adriatic southeastern coastal area is an eutrophic area that is strongly affected by freshwater inputs particularly from the Buna/ Bojana River system.en
dc.language.isoEnglishen
dc.relation.ispartofEstuarine, Coastal and Shelf Scienceen
dc.relation.ispartofseries/88 (2010)en
dc.subjecteutrophicationen
dc.subjectdissolved nutrientsen
dc.subjectcoastal stripen
dc.subjectAdriatic seaen
dc.subjecthydrodynamics regimeen
dc.titleIs the southeastern Adriatic Sea coastal strip an eutrophic area?en
dc.typearticleen
dc.description.statusPublisheden
dc.description.pagenumber395-406en
dc.subject.INGV03. Hydrosphere::03.04. Chemical and biological::03.04.04. Ecosystemsen
dc.description.obiettivoSpecifico1.8. Osservazioni di geofisica ambientaleen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorMarini, M.en
dc.contributor.authorGrilli, F.en
dc.contributor.authorGuarnieri, A.en
dc.contributor.authorBurton, H. J.en
dc.contributor.authorKlajic, Z.en
dc.contributor.authorPinardi, N.en
dc.contributor.authorSanxhaku, M.en
dc.contributor.departmentInstitue of Marine Science, National Research Centeren
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italiaen
dc.contributor.departmentUniversity of Southern California, Los Angelesen
dc.contributor.departmentInstitute of Marine Biology Kotor, Montenegroen
dc.contributor.departmentCIRSA, University of Bologna, Ravenna, Italyen
dc.contributor.departmentInstitute of Hydrometeorology, Tirana, Albaniaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextreserved-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptInstitute of Marine Science, National Research Council, Ancona, Italy-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Bologna, Bologna, Italia-
crisitem.author.deptUniversity of Southern California, Los Angeles-
crisitem.author.deptInstitute of Marine Biology Kotor, Montenegro-
crisitem.author.deptInstitute of Hydrometeorology, Tirana, Albania-
crisitem.author.orcid0000-0001-8162-6571-
crisitem.author.orcid0000-0003-4765-0775-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent03. Hydrosphere-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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