FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2611933969> ?p ?o ?g. }

• W2611933969 abstract "The general circulation in the northwestern Mediterranean Sea is characterized by a cyclonic circulation. The northern part of this gyre is formed by the Northern Current (NC), which flows along the continental slope from the Ligurian Sea towards the Catalan Shelf. The NC has an important influence on the Gulf of Lion (GoL), a large continental margin in the northern part of the basin. The NC constitutes an effective dynamical barrier which blocks coastal waters on the continental shelf. The western part of the GoL is a key region for regulating the outflow from the continental shelf to the Catalan Basin. These exchanges are mainly induced by partially ageostrophic processes originating from the interaction between the NC and mesoscale activity like meanders, filaments and eddies. Both GoL and Catalan shelf are characterized by an intense mesoscale activity. Eddies in the GoL are baroclinic structures extending throughout the mixed layer (30 to 50m), often elliptic in shape and about 20-30km in diameter. Catalan eddies are characterized by a vertical extension between 70 and 100m and a diameter of about 45km. The LAgrangian Transport EXperiment (LATEX, 2008-2011) was designed to study the mechanisms of formation of anticyclones in the western part of the GoL and their influence on cross-shelf exchanges. Mesoscale anticyclones have been observed in the western part of the GoL and over the Catalan shelf by the combined use of data from satellite observations, in situ measurements and numerical modeling. Recent numerical experiments show an anticyclonic circulation extending over a large part of the coastal area (latitudinal range : 41°50' to 43°N ; longitudinal range : 3°10' to 4°10'E). Interaction with a meander of the NC induces the separation of this circulation in two different eddies, one in the GoL and the other in the Catalan shelf. These eddies exhibit strong interaction between them, resulting in important exchanges between the two coastal regions. On one hand the Catalan eddy causes a heat transfer to the GoL; and, on the other hand, the interaction between the GoL eddy and a topographic barrier (Cap Creus) leads to a transfer of energy to the Catalan eddy. In order to quantify this exchange, a balance of kinetic energy has been analyzed from the model results. Numerical results are also discussed in comparison with in situ observations collected during the Latex09 campaign (August 24-28, 2009). The analysis of Sea Surface Temperature (SST) satellite images, Acoustic Doppler Current Profiler (ADCP) and Lagrangian drifter trajectories, confirmed the above interpretation derived from numerical model." @default.
• W2611933969 created "2017-05-12" @default.
• W2611933969 creator A5005372016 @default.
• W2611933969 creator A5010991394 @default.
• W2611933969 creator A5027595072 @default.
• W2611933969 creator A5031051940 @default.
• W2611933969 creator A5045862950 @default.
• W2611933969 creator A5085402847 @default.
• W2611933969 date "2012-04-22" @default.
• W2611933969 modified "2023-10-15" @default.
• W2611933969 title "Role of mesoscale eddies on exchanges between coastal regions" @default.
• W2611933969 hasPublicationYear "2012" @default.
• W2611933969 type Work @default.
• W2611933969 sameAs 2611933969 @default.
• W2611933969 citedByCount "0" @default.
• W2611933969 crossrefType "proceedings-article" @default.
• W2611933969 hasAuthorship W2611933969A5005372016 @default.
• W2611933969 hasAuthorship W2611933969A5010991394 @default.
• W2611933969 hasAuthorship W2611933969A5027595072 @default.
• W2611933969 hasAuthorship W2611933969A5031051940 @default.
• W2611933969 hasAuthorship W2611933969A5045862950 @default.
• W2611933969 hasAuthorship W2611933969A5085402847 @default.
• W2611933969 hasConcept C111368507 @default.
• W2611933969 hasConcept C127313418 @default.
• W2611933969 hasConcept C153294291 @default.
• W2611933969 hasConcept C179065325 @default.
• W2611933969 hasConcept C196558001 @default.
• W2611933969 hasConcept C205649164 @default.
• W2611933969 hasConcept C39432304 @default.
• W2611933969 hasConcept C40382383 @default.
• W2611933969 hasConcept C49204034 @default.
• W2611933969 hasConcept C62649853 @default.
• W2611933969 hasConceptScore W2611933969C111368507 @default.
• W2611933969 hasConceptScore W2611933969C127313418 @default.
• W2611933969 hasConceptScore W2611933969C153294291 @default.
• W2611933969 hasConceptScore W2611933969C179065325 @default.
• W2611933969 hasConceptScore W2611933969C196558001 @default.
• W2611933969 hasConceptScore W2611933969C205649164 @default.
• W2611933969 hasConceptScore W2611933969C39432304 @default.
• W2611933969 hasConceptScore W2611933969C40382383 @default.
• W2611933969 hasConceptScore W2611933969C49204034 @default.
• W2611933969 hasConceptScore W2611933969C62649853 @default.
• W2611933969 hasLocation W26119339691 @default.
• W2611933969 hasLocation W26119339692 @default.
• W2611933969 hasOpenAccess W2611933969 @default.
• W2611933969 hasPrimaryLocation W26119339691 @default.
• W2611933969 hasRelatedWork W139153353 @default.
• W2611933969 hasRelatedWork W2064193917 @default.
• W2611933969 hasRelatedWork W2378372156 @default.
• W2611933969 hasRelatedWork W2748952813 @default.
• W2611933969 hasRelatedWork W289559479 @default.
• W2611933969 hasRelatedWork W2980864800 @default.
• W2611933969 hasRelatedWork W3139950680 @default.
• W2611933969 hasRelatedWork W327400388 @default.
• W2611933969 hasRelatedWork W4200006094 @default.
• W2611933969 hasRelatedWork W787775643 @default.
• W2611933969 isParatext "false" @default.
• W2611933969 isRetracted "false" @default.
• W2611933969 magId "2611933969" @default.
• W2611933969 workType "article" @default.