FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2071490622> ?p ?o ?g. }

• W2071490622 endingPage "5480" @default.
• W2071490622 startingPage "5465" @default.
• W2071490622 abstract "The North Pacific has two vertical silica maxima. The well‐known intermediate maximum occurs between 2000 and 2500 m with a potential density relative to 2000 dbar of 36.90 in the northeastern Pacific. The deep maximum, which has not been observed extensively before, is found at or near the ocean bottom in the northern North Pacific in a narrow latitude range. Maps of silica on isopycnals which intersect the intermediate and bottom maxima show that the lowest silica is found in the western tropical North Pacific, suggesting a route for the spread of South Pacific water into the deep North Pacific. Low‐silica water is found along the western boundary of the North Pacific, with a separate broad tongue south of Hawaii. The highest silica on both isopycnals is in the northeast Pacific. A bottom maximum in the Cascadia Basin in the northeastern Pacific can be differentiated from both open‐ocean maxima. Four sources for the vertical maxima are considered: in situ dissolution of sinking particles, bottom sediment dissolution, hydrothermal venting, and upslope advection in the northeastern Pacific. Because not enough is known about any of these sources, only rough estimates of their contributions can be made. The bottom maximum is most likely to result from bottom sediment dissolution but requires a flux larger than some current direct estimates. The Cascadia Basin bottom maximum may result from both bottom sediment dissolution and hydrothermal venting. The intermediate maximum is likely to result primarily from dissolution of sinking particles. There is no quantitative estimate of the effect of possible upslope advection or enhancement of bottom fluxes due to the Columbia River outflow." @default.
• W2071490622 created "2016-06-24" @default.
• W2071490622 creator A5024700925 @default.
• W2071490622 creator A5069414807 @default.
• W2071490622 date "1992-04-15" @default.
• W2071490622 modified "2023-10-14" @default.
• W2071490622 title "The double silica maximum in the North Pacific" @default.
• W2071490622 cites W1978107220 @default.
• W2071490622 cites W1987982517 @default.
• W2071490622 cites W2007493419 @default.
• W2071490622 cites W2010181949 @default.
• W2071490622 cites W2016735661 @default.
• W2071490622 cites W2024228259 @default.
• W2071490622 cites W2034032223 @default.
• W2071490622 cites W2036466534 @default.
• W2071490622 cites W2041035582 @default.
• W2071490622 cites W2042091011 @default.
• W2071490622 cites W2050073845 @default.
• W2071490622 cites W2055956022 @default.
• W2071490622 cites W2057257632 @default.
• W2071490622 cites W2059983564 @default.
• W2071490622 cites W2063905977 @default.
• W2071490622 cites W2064361040 @default.
• W2071490622 cites W2078956978 @default.
• W2071490622 cites W2080100576 @default.
• W2071490622 cites W2095348384 @default.
• W2071490622 cites W2102228039 @default.
• W2071490622 cites W2115334653 @default.
• W2071490622 cites W2143974654 @default.
• W2071490622 cites W2220821452 @default.
• W2071490622 cites W2489827622 @default.
• W2071490622 doi "https://doi.org/10.1029/92jc00037" @default.
• W2071490622 hasPublicationYear "1992" @default.
• W2071490622 type Work @default.
• W2071490622 sameAs 2071490622 @default.
• W2071490622 citedByCount "69" @default.
• W2071490622 countsByYear W20714906222012 @default.
• W2071490622 countsByYear W20714906222013 @default.
• W2071490622 countsByYear W20714906222014 @default.
• W2071490622 countsByYear W20714906222015 @default.
• W2071490622 countsByYear W20714906222017 @default.
• W2071490622 countsByYear W20714906222018 @default.
• W2071490622 countsByYear W20714906222019 @default.
• W2071490622 countsByYear W20714906222020 @default.
• W2071490622 countsByYear W20714906222021 @default.
• W2071490622 countsByYear W20714906222022 @default.
• W2071490622 crossrefType "journal-article" @default.
• W2071490622 hasAuthorship W2071490622A5024700925 @default.
• W2071490622 hasAuthorship W2071490622A5069414807 @default.
• W2071490622 hasConcept C109007969 @default.
• W2071490622 hasConcept C111368507 @default.
• W2071490622 hasConcept C114793014 @default.
• W2071490622 hasConcept C121332964 @default.
• W2071490622 hasConcept C122523270 @default.
• W2071490622 hasConcept C122846477 @default.
• W2071490622 hasConcept C127313418 @default.
• W2071490622 hasConcept C13280743 @default.
• W2071490622 hasConcept C159985019 @default.
• W2071490622 hasConcept C191897082 @default.
• W2071490622 hasConcept C192562407 @default.
• W2071490622 hasConcept C204323151 @default.
• W2071490622 hasConcept C2780275952 @default.
• W2071490622 hasConcept C2816523 @default.
• W2071490622 hasConcept C5072599 @default.
• W2071490622 hasConcept C68709404 @default.
• W2071490622 hasConcept C75031826 @default.
• W2071490622 hasConcept C97355855 @default.
• W2071490622 hasConceptScore W2071490622C109007969 @default.
• W2071490622 hasConceptScore W2071490622C111368507 @default.
• W2071490622 hasConceptScore W2071490622C114793014 @default.
• W2071490622 hasConceptScore W2071490622C121332964 @default.
• W2071490622 hasConceptScore W2071490622C122523270 @default.
• W2071490622 hasConceptScore W2071490622C122846477 @default.
• W2071490622 hasConceptScore W2071490622C127313418 @default.
• W2071490622 hasConceptScore W2071490622C13280743 @default.
• W2071490622 hasConceptScore W2071490622C159985019 @default.
• W2071490622 hasConceptScore W2071490622C191897082 @default.
• W2071490622 hasConceptScore W2071490622C192562407 @default.
• W2071490622 hasConceptScore W2071490622C204323151 @default.
• W2071490622 hasConceptScore W2071490622C2780275952 @default.
• W2071490622 hasConceptScore W2071490622C2816523 @default.
• W2071490622 hasConceptScore W2071490622C5072599 @default.
• W2071490622 hasConceptScore W2071490622C68709404 @default.
• W2071490622 hasConceptScore W2071490622C75031826 @default.
• W2071490622 hasConceptScore W2071490622C97355855 @default.
• W2071490622 hasIssue "C4" @default.
• W2071490622 hasLocation W20714906221 @default.
• W2071490622 hasOpenAccess W2071490622 @default.
• W2071490622 hasPrimaryLocation W20714906221 @default.
• W2071490622 hasRelatedWork W2021518050 @default.
• W2071490622 hasRelatedWork W2060773539 @default.
• W2071490622 hasRelatedWork W2074184322 @default.
• W2071490622 hasRelatedWork W2079834616 @default.
• W2071490622 hasRelatedWork W2085770273 @default.
• W2071490622 hasRelatedWork W2092247795 @default.
• W2071490622 hasRelatedWork W2740016666 @default.
• W2071490622 hasRelatedWork W2787103121 @default.
• W2071490622 hasRelatedWork W3023493760 @default.

• next