FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2065844369> ?p ?o ?g. }

• W2065844369 endingPage "13" @default.
• W2065844369 startingPage "3" @default.
• W2065844369 abstract "The concentrations of a large number of naturally occurring radioactive and stable nuclides, those produced in nuclear reactions caused by cosmic radiation (and by energetic particles produced in radioactive disintegrations) and in nuclear decays of naturally occurring long-lived nuclides, have been measured in the past five decades in the marine environment. In many cases these nuclides serve as tracers for the study of physical, chemical and biological processes in the oceans. In this article, an overview of their sources and source functions is presented, and the potential and demonstrated usefulness of these nuclides with special emphasis on those produced by cosmic rays. The concentrations of cosmogenic nuclides in the oceans are nominally in the range of 10−5–10−1 dpm/l, with isotope/element ratios in the range of 10−18–10−12. Major technical advances in the past two decades have allowed their measurements to be done fairly reliably. The data base on the distribution of these tracers in the oceans is therefore growing steadily. Several radiotracers successfully provide chronology of sediments, corals and manganese nodules, but learning about large scale ocean circulation is another matter. We discuss that merely our ability to make measurements of a tracer in the marine environment is not sufficient to use it as an effective tracer for delineating the important oceanic variables. Tracer data must be examined in terms of ocean models. Constructing ocean models is an iterative process between data acquisition and model building, forcing model outputs to become compatible with the observations. The oceanic processes are very complex, exhibiting significant spatial and temporal variability on a wide range of scales. For the tracer data to be useful in developing meaningful coupled atmosphere–ocean circulation models, which may be considered as the goal of tracer studies, one would require three-dimensional tracer data with sufficient resolution in the horizontal direction. The latter are not available, except for 14C, where a considerable data base is growing as a result of recent WOCE (World Ocean Circulation Experiment) expeditions. It is gratifying to see that the cosmogenic radiotracer field is evolving from an academic curiosity in the 1950–1980s, to its present-day form wherein it aims to become an integral part of realistic atmosphere–ocean global circulation models." @default.
• W2065844369 created "2016-06-24" @default.
• W2065844369 creator A5056092131 @default.
• W2065844369 date "1999-09-01" @default.
• W2065844369 modified "2023-09-23" @default.
• W2065844369 title "An overview of five decades of studies of cosmic ray produced nuclides in oceans" @default.
• W2065844369 cites W1567602110 @default.
• W2065844369 cites W1586790202 @default.
• W2065844369 cites W1928205127 @default.
• W2065844369 cites W1976278501 @default.
• W2065844369 cites W1981130690 @default.
• W2065844369 cites W1993376818 @default.
• W2065844369 cites W1995675261 @default.
• W2065844369 cites W1996460824 @default.
• W2065844369 cites W1998625397 @default.
• W2065844369 cites W1999659619 @default.
• W2065844369 cites W2012053493 @default.
• W2065844369 cites W2012197996 @default.
• W2065844369 cites W2013183714 @default.
• W2065844369 cites W2013386346 @default.
• W2065844369 cites W2013668561 @default.
• W2065844369 cites W2016166410 @default.
• W2065844369 cites W2016417261 @default.
• W2065844369 cites W2019984710 @default.
• W2065844369 cites W2024766957 @default.
• W2065844369 cites W2028940036 @default.
• W2065844369 cites W2036501804 @default.
• W2065844369 cites W2051604588 @default.
• W2065844369 cites W2057126672 @default.
• W2065844369 cites W2065762723 @default.
• W2065844369 cites W2066429819 @default.
• W2065844369 cites W2066837538 @default.
• W2065844369 cites W2072649306 @default.
• W2065844369 cites W2074084195 @default.
• W2065844369 cites W2074364749 @default.
• W2065844369 cites W2078979836 @default.
• W2065844369 cites W2079915343 @default.
• W2065844369 cites W2081773485 @default.
• W2065844369 cites W2083813718 @default.
• W2065844369 cites W2088055037 @default.
• W2065844369 cites W2091524823 @default.
• W2065844369 cites W2093610928 @default.
• W2065844369 cites W2097264368 @default.
• W2065844369 cites W2127723083 @default.
• W2065844369 cites W2134380122 @default.
• W2065844369 cites W2143855233 @default.
• W2065844369 cites W2152443092 @default.
• W2065844369 cites W2168237454 @default.
• W2065844369 cites W2179983064 @default.
• W2065844369 cites W2292144380 @default.
• W2065844369 cites W2464320232 @default.
• W2065844369 cites W2469577676 @default.
• W2065844369 cites W4256528145 @default.
• W2065844369 doi "https://doi.org/10.1016/s0048-9697(99)00120-5" @default.
• W2065844369 hasPublicationYear "1999" @default.
• W2065844369 type Work @default.
• W2065844369 sameAs 2065844369 @default.
• W2065844369 citedByCount "19" @default.
• W2065844369 countsByYear W20658443692012 @default.
• W2065844369 countsByYear W20658443692017 @default.
• W2065844369 countsByYear W20658443692018 @default.
• W2065844369 countsByYear W20658443692019 @default.
• W2065844369 countsByYear W20658443692020 @default.
• W2065844369 countsByYear W20658443692021 @default.
• W2065844369 countsByYear W20658443692022 @default.
• W2065844369 countsByYear W20658443692023 @default.
• W2065844369 crossrefType "journal-article" @default.
• W2065844369 hasAuthorship W2065844369A5056092131 @default.
• W2065844369 hasConcept C101140149 @default.
• W2065844369 hasConcept C111309251 @default.
• W2065844369 hasConcept C111368507 @default.
• W2065844369 hasConcept C121332964 @default.
• W2065844369 hasConcept C127313418 @default.
• W2065844369 hasConcept C158973077 @default.
• W2065844369 hasConcept C159985019 @default.
• W2065844369 hasConcept C164304813 @default.
• W2065844369 hasConcept C172593403 @default.
• W2065844369 hasConcept C177571023 @default.
• W2065844369 hasConcept C185544564 @default.
• W2065844369 hasConcept C192562407 @default.
• W2065844369 hasConcept C1965285 @default.
• W2065844369 hasConcept C204323151 @default.
• W2065844369 hasConcept C2778863792 @default.
• W2065844369 hasConcept C39432304 @default.
• W2065844369 hasConcept C545943180 @default.
• W2065844369 hasConceptScore W2065844369C101140149 @default.
• W2065844369 hasConceptScore W2065844369C111309251 @default.
• W2065844369 hasConceptScore W2065844369C111368507 @default.
• W2065844369 hasConceptScore W2065844369C121332964 @default.
• W2065844369 hasConceptScore W2065844369C127313418 @default.
• W2065844369 hasConceptScore W2065844369C158973077 @default.
• W2065844369 hasConceptScore W2065844369C159985019 @default.
• W2065844369 hasConceptScore W2065844369C164304813 @default.
• W2065844369 hasConceptScore W2065844369C172593403 @default.
• W2065844369 hasConceptScore W2065844369C177571023 @default.
• W2065844369 hasConceptScore W2065844369C185544564 @default.
• W2065844369 hasConceptScore W2065844369C192562407 @default.
• W2065844369 hasConceptScore W2065844369C1965285 @default.

• next