FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1966873783> ?p ?o ?g. }

• W1966873783 endingPage "486" @default.
• W1966873783 startingPage "475" @default.
• W1966873783 abstract "A fully integrated ice-sheet and glacio-isostatic numerical model was run in order to investigate the crustal response to ice loading during the Late Weichselian glaciation of the Barents Sea. The model was used to examine the hypothesis that relative reductions in water depth, caused by glacio-isostatic uplift, may have aided ice growth from Scandinavia and High Arctic island archipelagos into the Barents Sea during the last glacial. Two experiments were designed in which the bedrock response to ice loading was examined: (i) complete and rapid glaciation of the Barents Sea when iceberg calving is curtailed except at the continental margin, and (ii) staged growth of ice in which ice sheets are allowed to ground at different water depths. Model results predict that glacially generated isostatic uplift, caused by an isostatic forebulge from loads on Scandinavia, Svalbard and other island archipelagos, affected the central Barents Sea during the early phase of glaciation. Isostatic uplift, combined with global sea-level fall, is predicted to have reduced sea level in parts of the central Barents Sea by up to 200 m. This reduction would have been sufficient to raise the sea floor of the Central Bank into a subaerial position. Such sea-floor emergence is conducive to the initiation of grounded ice growth in the central Barents Sea. The model indicates that, prior to its glaciation, the depth of the Central Deep would have been reduced from around 400 m to 200 m. Such uplift aided the migration of grounded ice from the central Barents Sea and Scandinavia into the Central Deep. We conclude that ice loading over Scandinavia and Arctic island archipelagos during the first stages of the Late Weichselian may have caused uplift within the central Barents Sea and aided the growth of ice across the entire Barents Shelf. Copyright © 2000 John Wiley & Sons, Ltd." @default.
• W1966873783 created "2016-06-24" @default.
• W1966873783 creator A5000303897 @default.
• W1966873783 creator A5064142260 @default.
• W1966873783 creator A5071686907 @default.
• W1966873783 date "2000-01-01" @default.
• W1966873783 modified "2023-09-28" @default.
• W1966873783 title "Modelling the influence of glacial isostasy on Late Weichselian ice-sheet growth in the Barents Sea" @default.
• W1966873783 cites W1498137216 @default.
• W1966873783 cites W1505645564 @default.
• W1966873783 cites W1620764883 @default.
• W1966873783 cites W1625313574 @default.
• W1966873783 cites W1663630586 @default.
• W1966873783 cites W1676983964 @default.
• W1966873783 cites W1678809943 @default.
• W1966873783 cites W1968402863 @default.
• W1966873783 cites W1982870945 @default.
• W1966873783 cites W2002356564 @default.
• W1966873783 cites W2002612837 @default.
• W1966873783 cites W2028946394 @default.
• W1966873783 cites W2032053405 @default.
• W1966873783 cites W2034639312 @default.
• W1966873783 cites W2056572327 @default.
• W1966873783 cites W2057076149 @default.
• W1966873783 cites W2058269537 @default.
• W1966873783 cites W2064076409 @default.
• W1966873783 cites W2081662319 @default.
• W1966873783 cites W2092736170 @default.
• W1966873783 cites W2094394939 @default.
• W1966873783 cites W2102002872 @default.
• W1966873783 cites W2104504396 @default.
• W1966873783 cites W2112038383 @default.
• W1966873783 cites W2122297914 @default.
• W1966873783 cites W2125283958 @default.
• W1966873783 cites W2157426825 @default.
• W1966873783 cites W2159510032 @default.
• W1966873783 cites W2280624662 @default.
• W1966873783 doi "https://doi.org/10.1002/1099-1417(200007)15:5<475::aid-jqs523>3.0.co;2-i" @default.
• W1966873783 hasPublicationYear "2000" @default.
• W1966873783 type Work @default.
• W1966873783 sameAs 1966873783 @default.
• W1966873783 citedByCount "11" @default.
• W1966873783 countsByYear W19668737832015 @default.
• W1966873783 countsByYear W19668737832017 @default.
• W1966873783 countsByYear W19668737832018 @default.
• W1966873783 countsByYear W19668737832020 @default.
• W1966873783 crossrefType "journal-article" @default.
• W1966873783 hasAuthorship W1966873783A5000303897 @default.
• W1966873783 hasAuthorship W1966873783A5064142260 @default.
• W1966873783 hasAuthorship W1966873783A5071686907 @default.
• W1966873783 hasConcept C109007969 @default.
• W1966873783 hasConcept C111368507 @default.
• W1966873783 hasConcept C114793014 @default.
• W1966873783 hasConcept C123750103 @default.
• W1966873783 hasConcept C127313418 @default.
• W1966873783 hasConcept C136894858 @default.
• W1966873783 hasConcept C139419234 @default.
• W1966873783 hasConcept C140711978 @default.
• W1966873783 hasConcept C142047668 @default.
• W1966873783 hasConcept C151730666 @default.
• W1966873783 hasConcept C15739521 @default.
• W1966873783 hasConcept C161798024 @default.
• W1966873783 hasConcept C16335420 @default.
• W1966873783 hasConcept C16942324 @default.
• W1966873783 hasConcept C180705331 @default.
• W1966873783 hasConcept C204207459 @default.
• W1966873783 hasConcept C77928131 @default.
• W1966873783 hasConceptScore W1966873783C109007969 @default.
• W1966873783 hasConceptScore W1966873783C111368507 @default.
• W1966873783 hasConceptScore W1966873783C114793014 @default.
• W1966873783 hasConceptScore W1966873783C123750103 @default.
• W1966873783 hasConceptScore W1966873783C127313418 @default.
• W1966873783 hasConceptScore W1966873783C136894858 @default.
• W1966873783 hasConceptScore W1966873783C139419234 @default.
• W1966873783 hasConceptScore W1966873783C140711978 @default.
• W1966873783 hasConceptScore W1966873783C142047668 @default.
• W1966873783 hasConceptScore W1966873783C151730666 @default.
• W1966873783 hasConceptScore W1966873783C15739521 @default.
• W1966873783 hasConceptScore W1966873783C161798024 @default.
• W1966873783 hasConceptScore W1966873783C16335420 @default.
• W1966873783 hasConceptScore W1966873783C16942324 @default.
• W1966873783 hasConceptScore W1966873783C180705331 @default.
• W1966873783 hasConceptScore W1966873783C204207459 @default.
• W1966873783 hasConceptScore W1966873783C77928131 @default.
• W1966873783 hasIssue "5" @default.
• W1966873783 hasLocation W19668737831 @default.
• W1966873783 hasOpenAccess W1966873783 @default.
• W1966873783 hasPrimaryLocation W19668737831 @default.
• W1966873783 hasRelatedWork W1966873783 @default.
• W1966873783 hasRelatedWork W1970174242 @default.
• W1966873783 hasRelatedWork W1986036340 @default.
• W1966873783 hasRelatedWork W2024688787 @default.
• W1966873783 hasRelatedWork W2106366209 @default.
• W1966873783 hasRelatedWork W2341202561 @default.
• W1966873783 hasRelatedWork W2626408974 @default.
• W1966873783 hasRelatedWork W3088812051 @default.
• W1966873783 hasRelatedWork W4244289313 @default.
• W1966873783 hasRelatedWork W793276886 @default.

• next