FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4225262009> ?p ?o ?g. }

• W4225262009 endingPage "564" @default.
• W4225262009 startingPage "549" @default.
• W4225262009 abstract "Abstract. Oceanic influences on shelf seas are mediated by flow along and across continental slopes, with consequences for regional hydrography and ecosystems. Here we present evidence for the variable North Atlantic influence on European shelf seas over the last 4 decades using ocean analysis and reanalysis products, as well as an eddy-resolving ocean model hindcast. To first order, flows oriented along isobaths at the continental slope are related to the poleward increase in density in the adjacent deep ocean that supports a geostrophic inflow towards the slope. In the North Atlantic, this density gradient and associated inflow have undergone substantial, sometimes abrupt, changes in recent decades. Inflow in the range 10–15 Sv is identified with eastward transport in temperature classes at 30∘ W in the latitude range 45–60∘ N. Associated with major subpolar warming around 1997, a cool and fresh branch of the Atlantic inflow was substantially reduced, while a warm and more saline inflow branch strengthened, with respective changes of the order of 5 Sv. Total inflow fell from ∼ 15 Sv pre-1997 to ∼ 10 Sv post-1997. In the model hindcast, particle tracking is used to trace the origins of poleward flows along the continental slope to the west of Ireland and Scotland before and after 1997. Backtracking particles up to 4 years, a range of subtropical and subpolar pathways is identified from a statistical perspective. In broad terms, cold, fresh waters of subpolar provenance were replaced by warm, saline waters of subtropical provenance. These changes have major implications for the downstream shelf regions that are strongly influenced by Atlantic inflow, in particular the northern North Sea, where “subtropicalization” of ecosystems has already been observed since the late 1990s." @default.
• W4225262009 created "2022-05-04" @default.
• W4225262009 creator A5000050692 @default.
• W4225262009 creator A5007527919 @default.
• W4225262009 creator A5021654467 @default.
• W4225262009 date "2022-05-02" @default.
• W4225262009 modified "2023-09-27" @default.
• W4225262009 title "Weakening and warming of the European Slope Current since the late 1990s attributed to basin-scale density changes" @default.
• W4225262009 cites W1967646619 @default.
• W4225262009 cites W1983801870 @default.
• W4225262009 cites W1989040884 @default.
• W4225262009 cites W1995764679 @default.
• W4225262009 cites W2005327544 @default.
• W4225262009 cites W2005612245 @default.
• W4225262009 cites W2008598417 @default.
• W4225262009 cites W2031566797 @default.
• W4225262009 cites W2042374286 @default.
• W4225262009 cites W2050168384 @default.
• W4225262009 cites W2059198684 @default.
• W4225262009 cites W2063435852 @default.
• W4225262009 cites W2075522895 @default.
• W4225262009 cites W2082865467 @default.
• W4225262009 cites W2095401211 @default.
• W4225262009 cites W2097863905 @default.
• W4225262009 cites W2107368401 @default.
• W4225262009 cites W2112816441 @default.
• W4225262009 cites W2114741599 @default.
• W4225262009 cites W2126301429 @default.
• W4225262009 cites W2153764913 @default.
• W4225262009 cites W2156505961 @default.
• W4225262009 cites W2169957563 @default.
• W4225262009 cites W2173251738 @default.
• W4225262009 cites W2174922334 @default.
• W4225262009 cites W2473336205 @default.
• W4225262009 cites W2509360153 @default.
• W4225262009 cites W2509871687 @default.
• W4225262009 cites W2510473887 @default.
• W4225262009 cites W2521826633 @default.
• W4225262009 cites W2612800205 @default.
• W4225262009 cites W2618718511 @default.
• W4225262009 cites W2806831817 @default.
• W4225262009 cites W2884122906 @default.
• W4225262009 cites W2891461053 @default.
• W4225262009 cites W2895933540 @default.
• W4225262009 cites W2896751458 @default.
• W4225262009 cites W2920192945 @default.
• W4225262009 cites W2970294764 @default.
• W4225262009 cites W3003494020 @default.
• W4225262009 cites W3015027266 @default.
• W4225262009 cites W4205272434 @default.
• W4225262009 cites W4232990077 @default.
• W4225262009 doi "https://doi.org/10.5194/os-18-549-2022" @default.
• W4225262009 hasPublicationYear "2022" @default.
• W4225262009 type Work @default.
• W4225262009 citedByCount "0" @default.
• W4225262009 crossrefType "journal-article" @default.
• W4225262009 hasAuthorship W4225262009A5000050692 @default.
• W4225262009 hasAuthorship W4225262009A5007527919 @default.
• W4225262009 hasAuthorship W4225262009A5021654467 @default.
• W4225262009 hasBestOaLocation W42252620091 @default.
• W4225262009 hasConcept C111368507 @default.
• W4225262009 hasConcept C127313418 @default.
• W4225262009 hasConcept C133877212 @default.
• W4225262009 hasConcept C184751465 @default.
• W4225262009 hasConcept C187599188 @default.
• W4225262009 hasConcept C2776132308 @default.
• W4225262009 hasConcept C49204034 @default.
• W4225262009 hasConcept C60069189 @default.
• W4225262009 hasConcept C76256466 @default.
• W4225262009 hasConcept C78091846 @default.
• W4225262009 hasConcept C83002819 @default.
• W4225262009 hasConceptScore W4225262009C111368507 @default.
• W4225262009 hasConceptScore W4225262009C127313418 @default.
• W4225262009 hasConceptScore W4225262009C133877212 @default.
• W4225262009 hasConceptScore W4225262009C184751465 @default.
• W4225262009 hasConceptScore W4225262009C187599188 @default.
• W4225262009 hasConceptScore W4225262009C2776132308 @default.
• W4225262009 hasConceptScore W4225262009C49204034 @default.
• W4225262009 hasConceptScore W4225262009C60069189 @default.
• W4225262009 hasConceptScore W4225262009C76256466 @default.
• W4225262009 hasConceptScore W4225262009C78091846 @default.
• W4225262009 hasConceptScore W4225262009C83002819 @default.
• W4225262009 hasFunder F4320334631 @default.
• W4225262009 hasIssue "2" @default.
• W4225262009 hasLocation W42252620091 @default.
• W4225262009 hasLocation W42252620092 @default.
• W4225262009 hasLocation W42252620093 @default.
• W4225262009 hasOpenAccess W4225262009 @default.
• W4225262009 hasPrimaryLocation W42252620091 @default.
• W4225262009 hasRelatedWork W1992996751 @default.
• W4225262009 hasRelatedWork W2053438434 @default.
• W4225262009 hasRelatedWork W2057080344 @default.
• W4225262009 hasRelatedWork W2511183000 @default.
• W4225262009 hasRelatedWork W2587683862 @default.
• W4225262009 hasRelatedWork W3087961845 @default.
• W4225262009 hasRelatedWork W4200053222 @default.
• W4225262009 hasRelatedWork W4233205298 @default.
• W4225262009 hasRelatedWork W4248882334 @default.

• next