FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1969706507> ?p ?o ?g. }

• W1969706507 abstract "Abstract. A new sediment transport model, considering currents, tides and waves is presented for the Adriatic Sea basin. The simulations concentrate on the winter of 2002–2003 because of field data availability and interesting intermittent processes occurrence. A process oriented analysis is performed to investigate the impact that Sirocco and Bora wind regimes have on sediment transport. The comparisons of the simulations with the observed data show that the model is capable to capture the main dynamics of sediment transport along the Italian coasts and the sediment concentration within the water column. This latter can reach values up to several g L−1, especially within the first centimetres above the bottom. The sediments are transported mainly southwards along the Italian coasts, consistently with the known literature results, except during Sirocco wind events, which can be responsible for reversing the coastal circulation in the northern area of the basin, and consequently the sediment transport. The resuspension of sediments is also related to the specific wave regimes induced by Bora and Sirocco, the former inducing resuspension events near the coasts while the latter causing a more diffused resuspension regime in the Northern Adriatic basin. Beside the realistic representation of short timescales resuspension/deposition events due to storms, the model was also used to investigate persistent erosion or deposition areas in the Adriatic Sea. Two main depocenters were identified: one, very pronounced, in the surroundings of the Po river delta, and another one a few kilometres off the coast in front of the Ancona promontory. A third region of accumulation, even if less intense, was found to be offshore the southernmost limit of the Gargano region. On the contrary the whole western coast within a distance of a few kilometres from the shore was found to be subject to prevailing erosion. The comparison with observed accumulation and erosion data shows that the model captures well the main depocenters in the domain and the erosion within the very coastal belt of the western side of the basin, but seems to be too erosive in a few areas, in particular those where the contribution of sediment inflow to the sea of some minor but intermittently important rivers is not considered in a realistic way as input to the model." @default.
• W1969706507 created "2016-06-24" @default.
• W1969706507 creator A5011545206 @default.
• W1969706507 creator A5059404839 @default.
• W1969706507 creator A5065557373 @default.
• W1969706507 creator A5069491379 @default.
• W1969706507 date "2014-06-06" @default.
• W1969706507 modified "2023-10-13" @default.
• W1969706507 title "Numerical modelling of sediment transport in the Adriatic Sea" @default.
• W1969706507 cites W1529100907 @default.
• W1969706507 cites W1549882949 @default.
• W1969706507 cites W1963788683 @default.
• W1969706507 cites W1969430019 @default.
• W1969706507 cites W1970739800 @default.
• W1969706507 cites W1981410591 @default.
• W1969706507 cites W1981669700 @default.
• W1969706507 cites W1986783416 @default.
• W1969706507 cites W1990227799 @default.
• W1969706507 cites W1992290310 @default.
• W1969706507 cites W1998512720 @default.
• W1969706507 cites W2000723799 @default.
• W1969706507 cites W2013720040 @default.
• W1969706507 cites W2014055600 @default.
• W1969706507 cites W2014124878 @default.
• W1969706507 cites W2028186785 @default.
• W1969706507 cites W2042651645 @default.
• W1969706507 cites W2067149672 @default.
• W1969706507 cites W2076483674 @default.
• W1969706507 cites W2076830172 @default.
• W1969706507 cites W2081269888 @default.
• W1969706507 cites W2089808190 @default.
• W1969706507 cites W2090375438 @default.
• W1969706507 cites W2091048250 @default.
• W1969706507 cites W2094624702 @default.
• W1969706507 cites W2097419181 @default.
• W1969706507 cites W2099190257 @default.
• W1969706507 cites W2099915250 @default.
• W1969706507 cites W2108369776 @default.
• W1969706507 cites W2113548869 @default.
• W1969706507 cites W2128500077 @default.
• W1969706507 cites W2128506685 @default.
• W1969706507 cites W2154063755 @default.
• W1969706507 cites W2154306139 @default.
• W1969706507 cites W2157292196 @default.
• W1969706507 cites W2159499458 @default.
• W1969706507 cites W2175751237 @default.
• W1969706507 cites W2196831689 @default.
• W1969706507 cites W2213245521 @default.
• W1969706507 doi "https://doi.org/10.5194/osd-11-1391-2014" @default.
• W1969706507 hasPublicationYear "2014" @default.
• W1969706507 type Work @default.
• W1969706507 sameAs 1969706507 @default.
• W1969706507 citedByCount "1" @default.
• W1969706507 countsByYear W19697065072023 @default.
• W1969706507 crossrefType "posted-content" @default.
• W1969706507 hasAuthorship W1969706507A5011545206 @default.
• W1969706507 hasAuthorship W1969706507A5059404839 @default.
• W1969706507 hasAuthorship W1969706507A5065557373 @default.
• W1969706507 hasAuthorship W1969706507A5069491379 @default.
• W1969706507 hasBestOaLocation W19697065071 @default.
• W1969706507 hasConcept C105306849 @default.
• W1969706507 hasConcept C109007969 @default.
• W1969706507 hasConcept C111368507 @default.
• W1969706507 hasConcept C114793014 @default.
• W1969706507 hasConcept C123157820 @default.
• W1969706507 hasConcept C127313418 @default.
• W1969706507 hasConcept C187320778 @default.
• W1969706507 hasConcept C18903297 @default.
• W1969706507 hasConcept C2779043415 @default.
• W1969706507 hasConcept C2816523 @default.
• W1969706507 hasConcept C4646841 @default.
• W1969706507 hasConcept C64297162 @default.
• W1969706507 hasConcept C65589250 @default.
• W1969706507 hasConcept C76886044 @default.
• W1969706507 hasConcept C86803240 @default.
• W1969706507 hasConceptScore W1969706507C105306849 @default.
• W1969706507 hasConceptScore W1969706507C109007969 @default.
• W1969706507 hasConceptScore W1969706507C111368507 @default.
• W1969706507 hasConceptScore W1969706507C114793014 @default.
• W1969706507 hasConceptScore W1969706507C123157820 @default.
• W1969706507 hasConceptScore W1969706507C127313418 @default.
• W1969706507 hasConceptScore W1969706507C187320778 @default.
• W1969706507 hasConceptScore W1969706507C18903297 @default.
• W1969706507 hasConceptScore W1969706507C2779043415 @default.
• W1969706507 hasConceptScore W1969706507C2816523 @default.
• W1969706507 hasConceptScore W1969706507C4646841 @default.
• W1969706507 hasConceptScore W1969706507C64297162 @default.
• W1969706507 hasConceptScore W1969706507C65589250 @default.
• W1969706507 hasConceptScore W1969706507C76886044 @default.
• W1969706507 hasConceptScore W1969706507C86803240 @default.
• W1969706507 hasLocation W19697065071 @default.
• W1969706507 hasOpenAccess W1969706507 @default.
• W1969706507 hasPrimaryLocation W19697065071 @default.
• W1969706507 hasRelatedWork W1992943688 @default.
• W1969706507 hasRelatedWork W1996370225 @default.
• W1969706507 hasRelatedWork W2042525910 @default.
• W1969706507 hasRelatedWork W2111536168 @default.
• W1969706507 hasRelatedWork W2210362217 @default.
• W1969706507 hasRelatedWork W2295835339 @default.
• W1969706507 hasRelatedWork W2330828760 @default.

• next