FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2330484996> ?p ?o ?g. }

• W2330484996 endingPage "266" @default.
• W2330484996 startingPage "257" @default.
• W2330484996 abstract "Abstract We examine the pattern of spreading of warm subtropical-origin waters around Greenland for the years 1992–2009 using a high-resolution (4km horizontal grid) coupled ocean and sea-ice simulation. The simulation, provided by the Estimating the Circulation and Climate of the Ocean, Phase II (ECCO2) project, qualitatively reproduces the observed warming of subsurface waters in the subpolar gyre associated with changes of the North Atlantic atmospheric state that occurred in the mid-1990s. The modeled subsurface ocean temperature warmed by 1.5˚C in southeast and southwest Greenland during 1994–2005 and subsequently cooled by 0.5˚C; modeled subsurface ocean temperature increased by 2–2.5˚C in central and then northwest Greenland during 1997–2005 and stabilized thereafter, while it increased after 2005 by <0.5˚C in north Greenland. Comparisons with in situ measurements off the continental shelf in the Labrador and Irminger Seas indicate that the model initial conditions were 0.4˚C too warm in the south but the simulated warming is correctly reproduced; while measurements from eastern Baffin Bay reveal that the model initial conditions were 1.0˚C too cold in the northwest but the simulated ocean warming brought modeled temperature closer to observations, i.e. the simulated warming is 1.0˚C too large. At several key locations, the modeled oceanic changes off the shelf and below the seasonal mixed layer were rapidly transmitted to the shelf within troughs towards (model-unresolved) fjords. Unless blocked in the fjords by shallow sills, these warm subsurface waters had potential to propagate down the fjords and melt the glacier fronts. Based on model sensitivity simulations from an independent study (Xu and others, 2012), we show that the oceanic changes have very likely increased the subaqueous melt rates of the glacier fronts, and in turn impacted the rates of glacier flow." @default.
• W2330484996 created "2016-06-24" @default.
• W2330484996 creator A5004110951 @default.
• W2330484996 creator A5054685597 @default.
• W2330484996 creator A5079862274 @default.
• W2330484996 creator A5086628877 @default.
• W2330484996 date "2012-01-01" @default.
• W2330484996 modified "2023-10-07" @default.
• W2330484996 title "Spreading of warm ocean waters around Greenland as a possible cause for glacier acceleration" @default.
• W2330484996 cites W1729123500 @default.
• W2330484996 cites W1809829952 @default.
• W2330484996 cites W1964998975 @default.
• W2330484996 cites W1968682222 @default.
• W2330484996 cites W1968909820 @default.
• W2330484996 cites W1971461775 @default.
• W2330484996 cites W1977528393 @default.
• W2330484996 cites W1983258892 @default.
• W2330484996 cites W1992652001 @default.
• W2330484996 cites W2004304922 @default.
• W2330484996 cites W2005786608 @default.
• W2330484996 cites W2007408843 @default.
• W2330484996 cites W2008589570 @default.
• W2330484996 cites W2012092742 @default.
• W2330484996 cites W2014035535 @default.
• W2330484996 cites W2024500585 @default.
• W2330484996 cites W2030563382 @default.
• W2330484996 cites W2043125375 @default.
• W2330484996 cites W2043976103 @default.
• W2330484996 cites W2057313876 @default.
• W2330484996 cites W2064458214 @default.
• W2330484996 cites W2078170471 @default.
• W2330484996 cites W2094558621 @default.
• W2330484996 cites W2104866858 @default.
• W2330484996 cites W2108808592 @default.
• W2330484996 cites W2115870595 @default.
• W2330484996 cites W2117558319 @default.
• W2330484996 cites W2121304076 @default.
• W2330484996 cites W2123027903 @default.
• W2330484996 cites W2124745617 @default.
• W2330484996 cites W2125370488 @default.
• W2330484996 cites W2131788414 @default.
• W2330484996 cites W2137816126 @default.
• W2330484996 cites W2138176285 @default.
• W2330484996 cites W2161306464 @default.
• W2330484996 cites W2163259012 @default.
• W2330484996 cites W2163841260 @default.
• W2330484996 cites W2179541677 @default.
• W2330484996 cites W2333209794 @default.
• W2330484996 doi "https://doi.org/10.3189/2012aog60a136" @default.
• W2330484996 hasPublicationYear "2012" @default.
• W2330484996 type Work @default.
• W2330484996 sameAs 2330484996 @default.
• W2330484996 citedByCount "92" @default.
• W2330484996 countsByYear W23304849962013 @default.
• W2330484996 countsByYear W23304849962014 @default.
• W2330484996 countsByYear W23304849962015 @default.
• W2330484996 countsByYear W23304849962016 @default.
• W2330484996 countsByYear W23304849962017 @default.
• W2330484996 countsByYear W23304849962018 @default.
• W2330484996 countsByYear W23304849962019 @default.
• W2330484996 countsByYear W23304849962020 @default.
• W2330484996 countsByYear W23304849962021 @default.
• W2330484996 countsByYear W23304849962022 @default.
• W2330484996 countsByYear W23304849962023 @default.
• W2330484996 crossrefType "journal-article" @default.
• W2330484996 hasAuthorship W2330484996A5004110951 @default.
• W2330484996 hasAuthorship W2330484996A5054685597 @default.
• W2330484996 hasAuthorship W2330484996A5079862274 @default.
• W2330484996 hasAuthorship W2330484996A5086628877 @default.
• W2330484996 hasBestOaLocation W23304849961 @default.
• W2330484996 hasConcept C100834320 @default.
• W2330484996 hasConcept C111368507 @default.
• W2330484996 hasConcept C114793014 @default.
• W2330484996 hasConcept C115880899 @default.
• W2330484996 hasConcept C123750103 @default.
• W2330484996 hasConcept C127313418 @default.
• W2330484996 hasConcept C135310875 @default.
• W2330484996 hasConcept C14168384 @default.
• W2330484996 hasConcept C17409809 @default.
• W2330484996 hasConcept C184751465 @default.
• W2330484996 hasConcept C187599188 @default.
• W2330484996 hasConcept C2780021526 @default.
• W2330484996 hasConcept C30380174 @default.
• W2330484996 hasConcept C40201923 @default.
• W2330484996 hasConcept C49204034 @default.
• W2330484996 hasConcept C505870484 @default.
• W2330484996 hasConcept C78091846 @default.
• W2330484996 hasConcept C86803240 @default.
• W2330484996 hasConceptScore W2330484996C100834320 @default.
• W2330484996 hasConceptScore W2330484996C111368507 @default.
• W2330484996 hasConceptScore W2330484996C114793014 @default.
• W2330484996 hasConceptScore W2330484996C115880899 @default.
• W2330484996 hasConceptScore W2330484996C123750103 @default.
• W2330484996 hasConceptScore W2330484996C127313418 @default.
• W2330484996 hasConceptScore W2330484996C135310875 @default.
• W2330484996 hasConceptScore W2330484996C14168384 @default.
• W2330484996 hasConceptScore W2330484996C17409809 @default.
• W2330484996 hasConceptScore W2330484996C184751465 @default.

• next