@prefix pubblicazioni: . @prefix unitaDiPersonaleInterno: . @prefix prodotto: . unitaDiPersonaleInterno:MATRICOLA5719 pubblicazioni:autoreCNRDi prodotto:ID49065 . @prefix prodottidellaricerca: . @prefix istituto: . istituto:CDS080 prodottidellaricerca:prodotto prodotto:ID49065 . @prefix modulo: . modulo:ID3966 prodottidellaricerca:prodotto prodotto:ID49065 . unitaDiPersonaleInterno:MATRICOLA6826 pubblicazioni:autoreCNRDi prodotto:ID49065 . unitaDiPersonaleInterno:MATRICOLA3602 pubblicazioni:autoreCNRDi prodotto:ID49065 . unitaDiPersonaleInterno:MATRICOLA16954 pubblicazioni:autoreCNRDi prodotto:ID49065 . @prefix rdf: . prodotto:ID49065 rdf:type prodotto:TIPO1101 . @prefix retescientifica: . prodotto:ID49065 rdf:type retescientifica:ProdottoDellaRicerca . @prefix rdfs: . prodotto:ID49065 rdfs:label "February 2003 marine atmospheric conditions and the bora over the northern Adriatic (Articolo in rivista)"@en . @prefix xsd: . prodotto:ID49065 pubblicazioni:anno "2006-01-01T00:00:00+01:00"^^xsd:gYear . @prefix skos: . prodotto:ID49065 skos:altLabel "
Dorman C.E.(1), Carniel S.(2), Cavaleri L.(2), Sclavo M.(2), Chiggiato J.(3), Doyle J.(4), Haack T.(4), Pullen J.(4), Grbec B.(5),Vilibic I.(5), Janekovic I.(6), Lee C.(7), Malacic V.(8), Orlic M.(9), Paschini E.(10), Russo A.(11), Signell R.P.(12) (2006)
February 2003 marine atmospheric conditions and the bora over the northern Adriatic
in Journal of geophysical research
"^^rdf:HTML ; pubblicazioni:autori "Dorman C.E.(1), Carniel S.(2), Cavaleri L.(2), Sclavo M.(2), Chiggiato J.(3), Doyle J.(4), Haack T.(4), Pullen J.(4), Grbec B.(5),Vilibic I.(5), Janekovic I.(6), Lee C.(7), Malacic V.(8), Orlic M.(9), Paschini E.(10), Russo A.(11), Signell R.P.(12)"^^xsd:string ; pubblicazioni:paginaInizio "C03S03"^^xsd:string ; pubblicazioni:altreInformazioni "Citation: Dorman, C. E., et al. (2006), February 2003 marine atmospheric conditions and the bora over the northern Adriatic, J. Geophys. Res., 111, C03S03, doi:10.1029/2005JC003134, [printed 112(C3), 2007]."^^xsd:string ; pubblicazioni:numeroVolume "111"^^xsd:string . @prefix ns11: . prodotto:ID49065 pubblicazioni:rivista ns11:ID388765 ; skos:note "ISI Web of Science (WOS)"^^xsd:string ; pubblicazioni:affiliazioni "(1)Scripps Institution of Oceanography & Geological Sciences Dept, UCSD, La Jolla & San Diego, CA, USA\n(2)Venice Section, Institute of Marine Sciences, National Research Council, Venice, Italy\n(3) Servizio IdroMeteorologico, Bologna, Italy\n(4) Marine Meteorology Div, Naval Research Lab, Monterey, CA, USA\n(5) Physical Oceanography Lab, Inst of Oceanography and Fisheries, Split, Croatia\n(6) Group for Satellite Oceanography, Center for Marine Res, Rudjer Boskovi Inst, Zagreb, Croatia\n(7) Applied Physics Lab, University of Washington, Seattle, WA, USA\n(8) National Institute of Biology, Marine Biology Station, Piran, Slovenia\n(9) Andrija Mohorovicic Geophysical Inst, University of Zagreb, Zagreb, Croatia\n(10) Ancona Section, Institute of Marine Sciences, National Research Council, Ancona, Italy\n(11) Dipartimento di Scienze del Mare, Universit\u00E0 Politecnica delle Marche, Ancona, Italy\n(12) NATO Undersea Research Centre, La Spezia, Italy"^^xsd:string ; pubblicazioni:titolo "February 2003 marine atmospheric conditions and the bora over the northern Adriatic"^^xsd:string ; prodottidellaricerca:abstract "A winter oceanographic field experiment provided an opportunity to examine the atmospheric marine conditions over the northern Adriatic. Mean February winds are from a north-easterly direction over most of the Adriatic and more northerly along the western coast. Wind speeds are fastest in jets over the NE coast during bora events and weakest in the mid-north-western Adriatic. Diurnal air temperature cycles are smallest on the NE coast and largest in the mid-western Adriatic. The maximum sea-air difference is +10 degrees C on the eastern coast and near zero on the mid-western Adriatic. Boras are north-easterly wind events that sweep off Croatia and Slovenia, bringing slightly colder and drier air over the northern Adriatic. Bora season is from December to March. Winter 2002\u00962003 was normal for bora events. Synoptic-scale temporal variations are correlated over the northern Adriatic. Wind stress is concentrated over the NE half of Adriatic in four bora jets, and weak in the NW Adriatic. There is significant variation in wind stress mean and standard deviation structure over the northern Adriatic with each bora event." ; prodottidellaricerca:prodottoDi istituto:CDS080 , modulo:ID3966 ; pubblicazioni:autoreCNR unitaDiPersonaleInterno:MATRICOLA5719 , unitaDiPersonaleInterno:MATRICOLA3602 , unitaDiPersonaleInterno:MATRICOLA16954 , unitaDiPersonaleInterno:MATRICOLA6826 . @prefix parolechiave: . prodotto:ID49065 parolechiave:insiemeDiParoleChiave . ns11:ID388765 pubblicazioni:rivistaDi prodotto:ID49065 . parolechiave:insiemeDiParoleChiaveDi prodotto:ID49065 .