FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2020133376> ?p ?o ?g. }

• W2020133376 endingPage "26723" @default.
• W2020133376 startingPage "26707" @default.
• W2020133376 abstract "Since 1980 the electrical conductivity method (ECM) has been used to infer volcanic acid signals in Greenland ice cores. The method reveals the great majority of major volcanic eruptions, including several known from historic records. Subsequent ion chromatographic analyses of the acid volcanic layers show the chemical composition, i.e., the concentration of the volcanic acids H 2 SO 4 , HCI, and HF plus, e.g., the nonvolcanically derived HNO 3 . While ECM data are available from a large number of shallow depth Greenland ice cores, covering the past 500–1500 years, only the Greenland Ice Core Project (GRIP), Greenland Ice Sheet Project 2 (GISP2), and Dye 3 deep ice cores exist for a detailed comparative study of volcanic signals in Greenland ice cores representing several thousand years. Comparison of the volcanic signals registered in the GRIP and GISP2 cores will be presented elsewhere. The latter cores were augered 30 km apart and essentially represent the same atmospheric conditions such as temperature, snow accumulation, and chemical composition of the air. Here we present a comparison between the major volcanic signals over the past 4000 years in the GRIP core from central Greenland and the Dye 3 core from SE Greenland in order to investigate the depositional differences. Many of the major signals are detected in both cores, but some of the differences in the records can be used to infer the latitudinal band of some eruption sites. Furthermore, the influence of the amount of annual precipitation and glaciological postdepositional processes on the volcanic signals is discussed." @default.
• W2020133376 created "2016-06-24" @default.
• W2020133376 creator A5031515138 @default.
• W2020133376 creator A5044458083 @default.
• W2020133376 creator A5054135883 @default.
• W2020133376 creator A5058714848 @default.
• W2020133376 creator A5061178593 @default.
• W2020133376 creator A5074592891 @default.
• W2020133376 creator A5091115110 @default.
• W2020133376 date "1997-11-30" @default.
• W2020133376 modified "2023-09-26" @default.
• W2020133376 title "A comparison of the volcanic records over the past 4000 years from the Greenland Ice Core Project and Dye 3 Greenland ice cores" @default.
• W2020133376 cites W1499073505 @default.
• W2020133376 cites W1552100204 @default.
• W2020133376 cites W1625027168 @default.
• W2020133376 cites W1636718234 @default.
• W2020133376 cites W1668335288 @default.
• W2020133376 cites W1672243584 @default.
• W2020133376 cites W1972688324 @default.
• W2020133376 cites W1982289088 @default.
• W2020133376 cites W1989300721 @default.
• W2020133376 cites W1993536958 @default.
• W2020133376 cites W1997832530 @default.
• W2020133376 cites W2003595495 @default.
• W2020133376 cites W2017354095 @default.
• W2020133376 cites W2017894968 @default.
• W2020133376 cites W2023347159 @default.
• W2020133376 cites W2044351448 @default.
• W2020133376 cites W2048256867 @default.
• W2020133376 cites W2053458539 @default.
• W2020133376 cites W2058875978 @default.
• W2020133376 cites W2063522701 @default.
• W2020133376 cites W2072977762 @default.
• W2020133376 cites W2082284070 @default.
• W2020133376 cites W2109927775 @default.
• W2020133376 cites W2128029627 @default.
• W2020133376 cites W2162929625 @default.
• W2020133376 cites W2169903549 @default.
• W2020133376 cites W2207412010 @default.
• W2020133376 cites W2486694309 @default.
• W2020133376 cites W4233100642 @default.
• W2020133376 cites W4235599414 @default.
• W2020133376 cites W4235747401 @default.
• W2020133376 cites W4238998056 @default.
• W2020133376 cites W4240677635 @default.
• W2020133376 cites W4243527208 @default.
• W2020133376 cites W4322391440 @default.
• W2020133376 cites W79311597 @default.
• W2020133376 doi "https://doi.org/10.1029/97jc00587" @default.
• W2020133376 hasPublicationYear "1997" @default.
• W2020133376 type Work @default.
• W2020133376 sameAs 2020133376 @default.
• W2020133376 citedByCount "175" @default.
• W2020133376 countsByYear W20201333762012 @default.
• W2020133376 countsByYear W20201333762013 @default.
• W2020133376 countsByYear W20201333762014 @default.
• W2020133376 countsByYear W20201333762015 @default.
• W2020133376 countsByYear W20201333762016 @default.
• W2020133376 countsByYear W20201333762017 @default.
• W2020133376 countsByYear W20201333762018 @default.
• W2020133376 countsByYear W20201333762019 @default.
• W2020133376 countsByYear W20201333762020 @default.
• W2020133376 countsByYear W20201333762022 @default.
• W2020133376 countsByYear W20201333762023 @default.
• W2020133376 crossrefType "journal-article" @default.
• W2020133376 hasAuthorship W2020133376A5031515138 @default.
• W2020133376 hasAuthorship W2020133376A5044458083 @default.
• W2020133376 hasAuthorship W2020133376A5054135883 @default.
• W2020133376 hasAuthorship W2020133376A5058714848 @default.
• W2020133376 hasAuthorship W2020133376A5061178593 @default.
• W2020133376 hasAuthorship W2020133376A5074592891 @default.
• W2020133376 hasAuthorship W2020133376A5091115110 @default.
• W2020133376 hasBestOaLocation W20201333761 @default.
• W2020133376 hasConcept C100970517 @default.
• W2020133376 hasConcept C111368507 @default.
• W2020133376 hasConcept C114793014 @default.
• W2020133376 hasConcept C120806208 @default.
• W2020133376 hasConcept C123750103 @default.
• W2020133376 hasConcept C127313418 @default.
• W2020133376 hasConcept C151730666 @default.
• W2020133376 hasConcept C197046000 @default.
• W2020133376 hasConcept C205325660 @default.
• W2020133376 hasConcept C205649164 @default.
• W2020133376 hasConcept C2779298566 @default.
• W2020133376 hasConcept C2780021526 @default.
• W2020133376 hasConcept C49204034 @default.
• W2020133376 hasConceptScore W2020133376C100970517 @default.
• W2020133376 hasConceptScore W2020133376C111368507 @default.
• W2020133376 hasConceptScore W2020133376C114793014 @default.
• W2020133376 hasConceptScore W2020133376C120806208 @default.
• W2020133376 hasConceptScore W2020133376C123750103 @default.
• W2020133376 hasConceptScore W2020133376C127313418 @default.
• W2020133376 hasConceptScore W2020133376C151730666 @default.
• W2020133376 hasConceptScore W2020133376C197046000 @default.
• W2020133376 hasConceptScore W2020133376C205325660 @default.
• W2020133376 hasConceptScore W2020133376C205649164 @default.
• W2020133376 hasConceptScore W2020133376C2779298566 @default.
• W2020133376 hasConceptScore W2020133376C2780021526 @default.

• next