FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2011398545> ?p ?o ?g. }

• W2011398545 endingPage "1424" @default.
• W2011398545 startingPage "1385" @default.
• W2011398545 abstract "An examination of the extensive hydrographic data sets collected by C.S.S. Hudson and F.S. Meteor in the Norwegian and Greenland Seas during February–June 1982 reveals property distributions and circulation patterns broadly similar to those seen in earlier data sets. These data sets, however, reveal the even stronger role played by topography, with evidence of separate circulation patterns and separate water masses in each of the deep basins. The high precision temperature, salinity and oxygen data obtained reveals significant differences in the deep and bottom waters found in the various basins of the Norwegian and Greenland Seas. A comparison of the 1982 data set with earlier sets shows that the renewal of Greenland Sea Deep Water must have taken place sometime over the last decade; however there is no evidence that deep convective renewal of any of the deep and bottom waters in this region was taking place at the time of the observations. The large-scale density fields, however, do suggest that deep convection to the bottom is most likely to occure in the Greenland Basin due to its deep cyclonic circulation. The hypothesis that Greenland Sea Deep Water (GSDW) is formed through dipycnal mixing processes acting on the warm salty core of Atlantic Water entering the Greenland Sea is examined. θ-S correlations and oxygen concentrations suggest that the salinity maxima in the Greenland Sea are the product of at least two separate mixing processes, not the hypothesized single mixing process leading to GSDW. A simple one-dimensional mixed layer model with ice growth and decay demonstrates that convective renewal of GSDW would have occurred within the Greenland Sea had the winter been a little more severe. The new GSDW produced would have only 0.003 less salt and less than 0.04 ml 1−1 greater oxygen concentration than that already in the basin. Consequently, detection of whether new deep water has been produced following a winter cooling season could be difficult even with the best of modern accuracy." @default.
• W2011398545 created "2016-06-24" @default.
• W2011398545 creator A5001830014 @default.
• W2011398545 creator A5005032096 @default.
• W2011398545 creator A5008599655 @default.
• W2011398545 creator A5042190551 @default.
• W2011398545 date "1990-09-01" @default.
• W2011398545 modified "2023-10-14" @default.
• W2011398545 title "The formation of Greenland Sea Deep Water: double diffusion or deep convection?" @default.
• W2011398545 cites W1984676558 @default.
• W2011398545 cites W1990572443 @default.
• W2011398545 cites W1997248427 @default.
• W2011398545 cites W1997677842 @default.
• W2011398545 cites W2009744985 @default.
• W2011398545 cites W2009960835 @default.
• W2011398545 cites W2017843511 @default.
• W2011398545 cites W2018679981 @default.
• W2011398545 cites W2025152168 @default.
• W2011398545 cites W2034254090 @default.
• W2011398545 cites W2055083075 @default.
• W2011398545 cites W2061885121 @default.
• W2011398545 cites W2076799159 @default.
• W2011398545 cites W2088877368 @default.
• W2011398545 cites W2135355688 @default.
• W2011398545 cites W2144150541 @default.
• W2011398545 cites W2175928457 @default.
• W2011398545 doi "https://doi.org/10.1016/0198-0149(90)90135-i" @default.
• W2011398545 hasPublicationYear "1990" @default.
• W2011398545 type Work @default.
• W2011398545 sameAs 2011398545 @default.
• W2011398545 citedByCount "66" @default.
• W2011398545 countsByYear W20113985452012 @default.
• W2011398545 countsByYear W20113985452013 @default.
• W2011398545 countsByYear W20113985452015 @default.
• W2011398545 countsByYear W20113985452016 @default.
• W2011398545 countsByYear W20113985452018 @default.
• W2011398545 countsByYear W20113985452019 @default.
• W2011398545 countsByYear W20113985452020 @default.
• W2011398545 countsByYear W20113985452021 @default.
• W2011398545 crossrefType "journal-article" @default.
• W2011398545 hasAuthorship W2011398545A5001830014 @default.
• W2011398545 hasAuthorship W2011398545A5005032096 @default.
• W2011398545 hasAuthorship W2011398545A5008599655 @default.
• W2011398545 hasAuthorship W2011398545A5042190551 @default.
• W2011398545 hasConcept C10899652 @default.
• W2011398545 hasConcept C111368507 @default.
• W2011398545 hasConcept C122846477 @default.
• W2011398545 hasConcept C127313418 @default.
• W2011398545 hasConcept C129513315 @default.
• W2011398545 hasConcept C140302290 @default.
• W2011398545 hasConcept C153294291 @default.
• W2011398545 hasConcept C157485413 @default.
• W2011398545 hasConcept C199641428 @default.
• W2011398545 hasConcept C202647207 @default.
• W2011398545 hasConcept C205649164 @default.
• W2011398545 hasConcept C21790881 @default.
• W2011398545 hasConcept C2780275952 @default.
• W2011398545 hasConcept C2988134249 @default.
• W2011398545 hasConcept C49204034 @default.
• W2011398545 hasConcept C6582778 @default.
• W2011398545 hasConcept C76256466 @default.
• W2011398545 hasConceptScore W2011398545C10899652 @default.
• W2011398545 hasConceptScore W2011398545C111368507 @default.
• W2011398545 hasConceptScore W2011398545C122846477 @default.
• W2011398545 hasConceptScore W2011398545C127313418 @default.
• W2011398545 hasConceptScore W2011398545C129513315 @default.
• W2011398545 hasConceptScore W2011398545C140302290 @default.
• W2011398545 hasConceptScore W2011398545C153294291 @default.
• W2011398545 hasConceptScore W2011398545C157485413 @default.
• W2011398545 hasConceptScore W2011398545C199641428 @default.
• W2011398545 hasConceptScore W2011398545C202647207 @default.
• W2011398545 hasConceptScore W2011398545C205649164 @default.
• W2011398545 hasConceptScore W2011398545C21790881 @default.
• W2011398545 hasConceptScore W2011398545C2780275952 @default.
• W2011398545 hasConceptScore W2011398545C2988134249 @default.
• W2011398545 hasConceptScore W2011398545C49204034 @default.
• W2011398545 hasConceptScore W2011398545C6582778 @default.
• W2011398545 hasConceptScore W2011398545C76256466 @default.
• W2011398545 hasIssue "9" @default.
• W2011398545 hasLocation W20113985451 @default.
• W2011398545 hasOpenAccess W2011398545 @default.
• W2011398545 hasPrimaryLocation W20113985451 @default.
• W2011398545 hasRelatedWork W1593834468 @default.
• W2011398545 hasRelatedWork W1971536038 @default.
• W2011398545 hasRelatedWork W2011398545 @default.
• W2011398545 hasRelatedWork W2029061368 @default.
• W2011398545 hasRelatedWork W2041834716 @default.
• W2011398545 hasRelatedWork W2052582380 @default.
• W2011398545 hasRelatedWork W2060201558 @default.
• W2011398545 hasRelatedWork W2062655224 @default.
• W2011398545 hasRelatedWork W2086789058 @default.
• W2011398545 hasRelatedWork W4212866415 @default.
• W2011398545 hasVolume "37" @default.
• W2011398545 isParatext "false" @default.
• W2011398545 isRetracted "false" @default.
• W2011398545 magId "2011398545" @default.
• W2011398545 workType "article" @default.