FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2013019218> ?p ?o ?g. }

• W2013019218 endingPage "73" @default.
• W2013019218 startingPage "62" @default.
• W2013019218 abstract "Strong vertical mixing in the Kuril Straits is believed to be an important contribution to the ventilation of the intermediate layer and water mass transformation in the North Pacific, especially for density greater than 27.1σθ. Furthermore, a recent modeling study has suggested that the vertical profile of vertical diffusivity is a key factor in the determination of thermohaline circulation in the North Pacific. Here we report the distribution of vertical diffusivity in the Bussol' Strait, the main conduit of water exchange and a possible central site of strong mixing in the Kuril Straits. Our analysis is based on a set of highly densed CTD observations, with a total of 127 casts across the strait in 2001. Vigorous density inversions occurred in the strait with the largest vertical displacement being over 250 m. We estimated the vertical diffusivity coefficient Kρ from the Thorpe scale for all the CTD data. The vertical average of Kρ estimated from all the casts is 60×10−4 m2 s−1. Overall, Kρ is relatively small in the upper 300 m (density range approximately 26.5–26.7σθ), whereas it is relatively large below a depth of 500 m (density range of >26.8σθ), with a maximum at the depths of 1100–1700 m. The distributions of Kρ and the amplitude of the diurnal tidal current are similar, suggesting that the mixing is caused by the strong diurnal tidal current. The amplification of the diurnal (tidal) current over slopes near the bottom causes the Kρ maximum at depths of ∼1100–1700m. We also introduce an empirical relationship between Kρ and the amplitude of the diurnal tidal current. The vertical diffusivity is one order of magnitude larger at the spring tide than at the neap tide, suggesting that there is extremely large variability of tidal mixing with the fortnightly modulation. In the intermediate layer at densities of 27.3–27.6σθ, large Kρ values (>60×10−4m2s−1) corresponds well to the colder and less-saline water mass characterized in the Bussol' Strait, confirming that water mass transformation occurs locally in the strait through strong diapycnal mixing." @default.
• W2013019218 created "2016-06-24" @default.
• W2013019218 creator A5000940896 @default.
• W2013019218 creator A5022662445 @default.
• W2013019218 creator A5025550652 @default.
• W2013019218 creator A5060663913 @default.
• W2013019218 creator A5068672332 @default.
• W2013019218 creator A5090207777 @default.
• W2013019218 date "2013-09-01" @default.
• W2013019218 modified "2023-10-13" @default.
• W2013019218 title "Distribution of vertical diffusivity in the Bussol' Strait: A mixing hot spot in the North Pacific" @default.
• W2013019218 cites W1694999744 @default.
• W2013019218 cites W1949939209 @default.
• W2013019218 cites W1981988359 @default.
• W2013019218 cites W1985812017 @default.
• W2013019218 cites W1986178578 @default.
• W2013019218 cites W1986691129 @default.
• W2013019218 cites W1987877406 @default.
• W2013019218 cites W1994752801 @default.
• W2013019218 cites W2000662520 @default.
• W2013019218 cites W2008675271 @default.
• W2013019218 cites W2013981258 @default.
• W2013019218 cites W2026212763 @default.
• W2013019218 cites W2031856122 @default.
• W2013019218 cites W2039203233 @default.
• W2013019218 cites W2040596784 @default.
• W2013019218 cites W2041996054 @default.
• W2013019218 cites W2043902623 @default.
• W2013019218 cites W2045515031 @default.
• W2013019218 cites W2049706000 @default.
• W2013019218 cites W2052968556 @default.
• W2013019218 cites W2055381657 @default.
• W2013019218 cites W2059179992 @default.
• W2013019218 cites W2068204246 @default.
• W2013019218 cites W2084690561 @default.
• W2013019218 cites W2085307553 @default.
• W2013019218 cites W2087846982 @default.
• W2013019218 cites W2094444584 @default.
• W2013019218 cites W2095197248 @default.
• W2013019218 cites W2135257859 @default.
• W2013019218 cites W2136995547 @default.
• W2013019218 cites W2172679823 @default.
• W2013019218 cites W2176197676 @default.
• W2013019218 doi "https://doi.org/10.1016/j.dsr.2013.05.010" @default.
• W2013019218 hasPublicationYear "2013" @default.
• W2013019218 type Work @default.
• W2013019218 sameAs 2013019218 @default.
• W2013019218 citedByCount "11" @default.
• W2013019218 countsByYear W20130192182014 @default.
• W2013019218 countsByYear W20130192182017 @default.
• W2013019218 countsByYear W20130192182018 @default.
• W2013019218 countsByYear W20130192182019 @default.
• W2013019218 countsByYear W20130192182020 @default.
• W2013019218 countsByYear W20130192182021 @default.
• W2013019218 countsByYear W20130192182023 @default.
• W2013019218 crossrefType "journal-article" @default.
• W2013019218 hasAuthorship W2013019218A5000940896 @default.
• W2013019218 hasAuthorship W2013019218A5022662445 @default.
• W2013019218 hasAuthorship W2013019218A5025550652 @default.
• W2013019218 hasAuthorship W2013019218A5060663913 @default.
• W2013019218 hasAuthorship W2013019218A5068672332 @default.
• W2013019218 hasAuthorship W2013019218A5090207777 @default.
• W2013019218 hasConcept C111368507 @default.
• W2013019218 hasConcept C114793014 @default.
• W2013019218 hasConcept C121332964 @default.
• W2013019218 hasConcept C127313418 @default.
• W2013019218 hasConcept C138777275 @default.
• W2013019218 hasConcept C140302290 @default.
• W2013019218 hasConcept C148043351 @default.
• W2013019218 hasConcept C159985019 @default.
• W2013019218 hasConcept C180205008 @default.
• W2013019218 hasConcept C192562407 @default.
• W2013019218 hasConcept C203496682 @default.
• W2013019218 hasConcept C204323151 @default.
• W2013019218 hasConcept C2780759522 @default.
• W2013019218 hasConcept C37668627 @default.
• W2013019218 hasConcept C49204034 @default.
• W2013019218 hasConcept C62520636 @default.
• W2013019218 hasConcept C91586092 @default.
• W2013019218 hasConceptScore W2013019218C111368507 @default.
• W2013019218 hasConceptScore W2013019218C114793014 @default.
• W2013019218 hasConceptScore W2013019218C121332964 @default.
• W2013019218 hasConceptScore W2013019218C127313418 @default.
• W2013019218 hasConceptScore W2013019218C138777275 @default.
• W2013019218 hasConceptScore W2013019218C140302290 @default.
• W2013019218 hasConceptScore W2013019218C148043351 @default.
• W2013019218 hasConceptScore W2013019218C159985019 @default.
• W2013019218 hasConceptScore W2013019218C180205008 @default.
• W2013019218 hasConceptScore W2013019218C192562407 @default.
• W2013019218 hasConceptScore W2013019218C203496682 @default.
• W2013019218 hasConceptScore W2013019218C204323151 @default.
• W2013019218 hasConceptScore W2013019218C2780759522 @default.
• W2013019218 hasConceptScore W2013019218C37668627 @default.
• W2013019218 hasConceptScore W2013019218C49204034 @default.
• W2013019218 hasConceptScore W2013019218C62520636 @default.
• W2013019218 hasConceptScore W2013019218C91586092 @default.
• W2013019218 hasFunder F4320320907 @default.
• W2013019218 hasFunder F4320320912 @default.

• next