FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2063716897> ?p ?o ?g. }

• W2063716897 endingPage "907" @default.
• W2063716897 startingPage "897" @default.
• W2063716897 abstract "The hydrological impact of the massive iceberg discharges during Heinrich events has been quantified for Heinrich 4 about 37 kyr ago. This event took place in a context of relatively stable orbital forcing and global ice volume. In this article, we propose to quantify the hydrological impact of the Heinrich event 1 which occurred at about 16 kyr BP. This time period is particularly interesting because orbital forcing was strong and it marks the onset of the last deglaciation. The results obtained here show that Heinrich event 1 has a larger isotopic amplitude than Heinrich event 4 when considering the cores located near the melting source. Concerning surface circulation, the northward progression of the North Atlantic Drift is affected only by Heinrich event 4, possibly because of the latitudinal extension of the melting area during this event. To cite this article: E. Cortijo et al., C. R. Geoscience 337 (2005). L'impact hydrologique des décharges massives d'icebergs liées aux événements de Heinrich a été quantifié pour l'événement de Heinrich 4, datant d'environ 37 ka BP, dans un contexte de relative stabilité des paramètres orbitaux et du volume global de glace. Dans cette note, nous proposons de quantifier l'impact hydrologique de l'événement de Heinrich 1, il y a 16 ka BP, qui s'est déroulé au début de la dernière déglaciation, sous des conditions de forçage orbital très différent. Les résultats montrent que l'amplitude isotopique de l'événement de Heinrich 1 est plus grande que celle de l'événement de Heinrich 4, lorsqu'on se place à proximité des sources de fonte. En revanche, la dérive nord-atlantique n'est affectée que pendant l'événement de Heinrich 4, vraisemblablement à cause de la disposition latitudinale de la langue de fonte pendant cet événement. Pour citer cet article : E. Cortijo et al., C. R. Geoscience 337 (2005)." @default.
• W2063716897 created "2016-06-24" @default.
• W2063716897 creator A5008755241 @default.
• W2063716897 creator A5021516314 @default.
• W2063716897 creator A5024126023 @default.
• W2063716897 creator A5039181593 @default.
• W2063716897 creator A5055902382 @default.
• W2063716897 date "2005-08-01" @default.
• W2063716897 modified "2023-09-30" @default.
• W2063716897 title "Heinrich events: hydrological impact" @default.
• W2063716897 cites W1504053044 @default.
• W2063716897 cites W1575505905 @default.
• W2063716897 cites W1768592839 @default.
• W2063716897 cites W1927648166 @default.
• W2063716897 cites W1964831585 @default.
• W2063716897 cites W1967286558 @default.
• W2063716897 cites W1968721411 @default.
• W2063716897 cites W1973227610 @default.
• W2063716897 cites W1976733971 @default.
• W2063716897 cites W1977660831 @default.
• W2063716897 cites W1979036030 @default.
• W2063716897 cites W1981028614 @default.
• W2063716897 cites W1985322823 @default.
• W2063716897 cites W1992799854 @default.
• W2063716897 cites W1994774798 @default.
• W2063716897 cites W2000469323 @default.
• W2063716897 cites W2001134294 @default.
• W2063716897 cites W2006652966 @default.
• W2063716897 cites W2007257396 @default.
• W2063716897 cites W2022716702 @default.
• W2063716897 cites W2032695494 @default.
• W2063716897 cites W2039667302 @default.
• W2063716897 cites W2039819271 @default.
• W2063716897 cites W2046913473 @default.
• W2063716897 cites W2051559013 @default.
• W2063716897 cites W2070221850 @default.
• W2063716897 cites W2074527287 @default.
• W2063716897 cites W2076339132 @default.
• W2063716897 cites W2089697716 @default.
• W2063716897 cites W2093419199 @default.
• W2063716897 cites W2099826005 @default.
• W2063716897 cites W2161365912 @default.
• W2063716897 cites W2216966513 @default.
• W2063716897 cites W2285770223 @default.
• W2063716897 cites W2296889313 @default.
• W2063716897 cites W2467664111 @default.
• W2063716897 cites W2762086252 @default.
• W2063716897 cites W2787092291 @default.
• W2063716897 cites W368140503 @default.
• W2063716897 cites W653466241 @default.
• W2063716897 doi "https://doi.org/10.1016/j.crte.2005.04.011" @default.
• W2063716897 hasPublicationYear "2005" @default.
• W2063716897 type Work @default.
• W2063716897 sameAs 2063716897 @default.
• W2063716897 citedByCount "20" @default.
• W2063716897 countsByYear W20637168972012 @default.
• W2063716897 countsByYear W20637168972013 @default.
• W2063716897 countsByYear W20637168972014 @default.
• W2063716897 countsByYear W20637168972015 @default.
• W2063716897 countsByYear W20637168972018 @default.
• W2063716897 countsByYear W20637168972020 @default.
• W2063716897 crossrefType "journal-article" @default.
• W2063716897 hasAuthorship W2063716897A5008755241 @default.
• W2063716897 hasAuthorship W2063716897A5021516314 @default.
• W2063716897 hasAuthorship W2063716897A5024126023 @default.
• W2063716897 hasAuthorship W2063716897A5039181593 @default.
• W2063716897 hasAuthorship W2063716897A5055902382 @default.
• W2063716897 hasBestOaLocation W20637168972 @default.
• W2063716897 hasConcept C127313418 @default.
• W2063716897 hasConcept C151730666 @default.
• W2063716897 hasConcept C15739521 @default.
• W2063716897 hasConcept C180705331 @default.
• W2063716897 hasConcept C2779343474 @default.
• W2063716897 hasConceptScore W2063716897C127313418 @default.
• W2063716897 hasConceptScore W2063716897C151730666 @default.
• W2063716897 hasConceptScore W2063716897C15739521 @default.
• W2063716897 hasConceptScore W2063716897C180705331 @default.
• W2063716897 hasConceptScore W2063716897C2779343474 @default.
• W2063716897 hasIssue "10-11" @default.
• W2063716897 hasLocation W20637168971 @default.
• W2063716897 hasLocation W20637168972 @default.
• W2063716897 hasLocation W20637168973 @default.
• W2063716897 hasLocation W20637168974 @default.
• W2063716897 hasLocation W20637168975 @default.
• W2063716897 hasLocation W20637168976 @default.
• W2063716897 hasOpenAccess W2063716897 @default.
• W2063716897 hasPrimaryLocation W20637168971 @default.
• W2063716897 hasRelatedWork W2003581071 @default.
• W2063716897 hasRelatedWork W2014303036 @default.
• W2063716897 hasRelatedWork W2048761473 @default.
• W2063716897 hasRelatedWork W2055763576 @default.
• W2063716897 hasRelatedWork W2076805175 @default.
• W2063716897 hasRelatedWork W2079868346 @default.
• W2063716897 hasRelatedWork W2170128802 @default.
• W2063716897 hasRelatedWork W3034610080 @default.
• W2063716897 hasRelatedWork W3088812051 @default.
• W2063716897 hasRelatedWork W4365458801 @default.
• W2063716897 hasVolume "337" @default.

• next