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Large Variability of Dissolved Inorganic Radiocarbon in the Kuroshio Extension of the Northwest North Pacific

Bibliographic Data

ID9245237
AuthorsLing Ding (0000-0002-2348-1076), Tiantian Ge, Huiwang Gao (0000-0002-4274-0811), Chunle Luo, Yuejun Xue, Ellen R M Druffel (0000-0002-7139-1075), Xuchen Wang (0009-0000-6093-3687)
Year2018
Volume60
Issue2
Pages691-704
Publication date2018-04-01
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueRadiocarbon (JOURNAL)
Journal identifiersISSN: 0033-8222 • E-ISSN: 1945-5755
PublisherCambridge University Press (CUP) (PUBLISHER)
DOI10.1017/rdc.2017.143
OpenAlexW2783071963
LanguageEN
References cited42

Radiocarbon ( 14 C) in dissolved inorganic carbon (DIC) was measured for water samples collected from six deep stations in the Kuroshio Extension (KE) region in the northwestern North Pacific in April–May 2015. Vertical profiles of Δ 14 C-DIC indicate that bomb-produced 14 C was present from the surface to ~1500 m water depth. Large variations in Δ 14 C-DIC values (300‰) were observed at 500 m water depth among the stations and the differences were likely controlled by transport and mixing dynamics of different water masses in the region. The major Pacific western boundary currents, such as Kuroshio and Oyashio and regional mesoscale eddies, could play important roles affecting the observed Δ 14 C-DIC variability. The depth profiles of both Δ 14 C-DIC and DIC concentrations can be predicted by the solution mixing model and can be used as conservative tracers of water mass movement and water parcel homogenization in the ocean

Boundary current · Deep water · Dissolved organic carbon · Mesoscale meteorology · Nutrient · Ocean current · Pacific ocean · Photic zone · Phytoplankton · Radiocarbon dating · Surface water · Water mass · Chemistry · Environmental Science · Geology and Paleoclimatology Research · Isotope Analysis in Ecology · Marine and coastal ecosystems · Geology · Oceanography

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Highly citedNo

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