FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2104091736> ?p ?o ?g. }

• W2104091736 endingPage "1538" @default.
• W2104091736 startingPage "1520" @default.
• W2104091736 abstract "Abstract The processes maintaining stratification in the oceanic middepth (between approximately 1000 and 3000 m) are explored using an eddy-resolving general circulation model composed of a two-hemisphere, semienclosed basin with a zonal reentrant channel in the southernmost eighth of the domain. The middepth region lies below the wind-driven main thermocline but above the diffusively driven abyssal ocean. Here, it is argued that middepth stratification is determined primarily in the model’s Antarctic Circumpolar Current. Competition between mean and eddy overturning in the channel leads to steeper isotherms and thus deeper stratification throughout the basin than would exist without the channel. Isotherms that outcrop only in the channel are nearly horizontal in the semienclosed portion of the domain, whereas isotherms that also outcrop in the Northern Hemisphere deviate from horizontal and are accompanied by geostrophically balanced meridional transport. A northern source of deep water (water with temperatures in the range of those in the channel) leads to the formation of a thick middepth thermostad. Changes in wind forcing over the channel influence the stratification throughout the domain. Since the middepth stratification is controlled by adiabatic dynamics in the channel, it becomes independent of the interior diffusivity κ as κ → 0. The meridional overturning circulation (MOC), as diagnosed by the mean meridional volume transport, also shows a tendency to become independent of κ as κ → 0, whereas the MOC diagnosed by water mass transport shows a continuing dependence on κ as κ → 0. A nonlocal scaling for MOC is developed that relates the strength of the northern MOC to the depth of isotherms in the southern channel. The results of this paper compare favorably to observations of large-scale neutral density in the World Ocean." @default.
• W2104091736 created "2016-06-24" @default.
• W2104091736 creator A5046068891 @default.
• W2104091736 creator A5073798785 @default.
• W2104091736 date "2010-07-01" @default.
• W2104091736 modified "2023-10-01" @default.
• W2104091736 title "What Sets the Strength of the Middepth Stratification and Overturning Circulation in Eddying Ocean Models?" @default.
• W2104091736 cites W1546816274 @default.
• W2104091736 cites W1837057137 @default.
• W2104091736 cites W1966114712 @default.
• W2104091736 cites W1971296939 @default.
• W2104091736 cites W1972028164 @default.
• W2104091736 cites W1976977540 @default.
• W2104091736 cites W1979878372 @default.
• W2104091736 cites W1988139802 @default.
• W2104091736 cites W1998382501 @default.
• W2104091736 cites W2007074215 @default.
• W2104091736 cites W2007104457 @default.
• W2104091736 cites W2009347438 @default.
• W2104091736 cites W2009554926 @default.
• W2104091736 cites W2010675915 @default.
• W2104091736 cites W2012214519 @default.
• W2104091736 cites W2022381979 @default.
• W2104091736 cites W2028387065 @default.
• W2104091736 cites W2033267016 @default.
• W2104091736 cites W2043735723 @default.
• W2104091736 cites W2044130592 @default.
• W2104091736 cites W2045016819 @default.
• W2104091736 cites W2057313876 @default.
• W2104091736 cites W2059670821 @default.
• W2104091736 cites W2074771503 @default.
• W2104091736 cites W2080723441 @default.
• W2104091736 cites W2093164547 @default.
• W2104091736 cites W2103710456 @default.
• W2104091736 cites W2108010418 @default.
• W2104091736 cites W2110491966 @default.
• W2104091736 cites W2110607246 @default.
• W2104091736 cites W2119347382 @default.
• W2104091736 cites W2121992961 @default.
• W2104091736 cites W2125138311 @default.
• W2104091736 cites W2132413642 @default.
• W2104091736 cites W2134866867 @default.
• W2104091736 cites W2139604512 @default.
• W2104091736 cites W2165757422 @default.
• W2104091736 cites W2168939336 @default.
• W2104091736 cites W2174279725 @default.
• W2104091736 cites W2177633214 @default.
• W2104091736 cites W2180546878 @default.
• W2104091736 cites W4232473186 @default.
• W2104091736 doi "https://doi.org/10.1175/2010jpo4393.1" @default.
• W2104091736 hasPublicationYear "2010" @default.
• W2104091736 type Work @default.
• W2104091736 sameAs 2104091736 @default.
• W2104091736 citedByCount "88" @default.
• W2104091736 countsByYear W21040917362012 @default.
• W2104091736 countsByYear W21040917362013 @default.
• W2104091736 countsByYear W21040917362014 @default.
• W2104091736 countsByYear W21040917362015 @default.
• W2104091736 countsByYear W21040917362016 @default.
• W2104091736 countsByYear W21040917362017 @default.
• W2104091736 countsByYear W21040917362018 @default.
• W2104091736 countsByYear W21040917362019 @default.
• W2104091736 countsByYear W21040917362020 @default.
• W2104091736 countsByYear W21040917362021 @default.
• W2104091736 countsByYear W21040917362022 @default.
• W2104091736 countsByYear W21040917362023 @default.
• W2104091736 crossrefType "journal-article" @default.
• W2104091736 hasAuthorship W2104091736A5046068891 @default.
• W2104091736 hasAuthorship W2104091736A5073798785 @default.
• W2104091736 hasBestOaLocation W21040917362 @default.
• W2104091736 hasConcept C100701293 @default.
• W2104091736 hasConcept C104196234 @default.
• W2104091736 hasConcept C105824904 @default.
• W2104091736 hasConcept C111368507 @default.
• W2104091736 hasConcept C121332964 @default.
• W2104091736 hasConcept C122846477 @default.
• W2104091736 hasConcept C127313418 @default.
• W2104091736 hasConcept C129513315 @default.
• W2104091736 hasConcept C14168384 @default.
• W2104091736 hasConcept C179065325 @default.
• W2104091736 hasConcept C187599188 @default.
• W2104091736 hasConcept C192943249 @default.
• W2104091736 hasConcept C196558001 @default.
• W2104091736 hasConcept C30380174 @default.
• W2104091736 hasConcept C3527866 @default.
• W2104091736 hasConcept C505870484 @default.
• W2104091736 hasConcept C5072599 @default.
• W2104091736 hasConcept C56905729 @default.
• W2104091736 hasConcept C57879066 @default.
• W2104091736 hasConcept C59822182 @default.
• W2104091736 hasConcept C76256466 @default.
• W2104091736 hasConcept C78091846 @default.
• W2104091736 hasConcept C86803240 @default.
• W2104091736 hasConcept C88548481 @default.
• W2104091736 hasConcept C97355855 @default.
• W2104091736 hasConceptScore W2104091736C100701293 @default.
• W2104091736 hasConceptScore W2104091736C104196234 @default.
• W2104091736 hasConceptScore W2104091736C105824904 @default.

• next