FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2074440415> ?p ?o ?g. }

• W2074440415 endingPage "595" @default.
• W2074440415 startingPage "582" @default.
• W2074440415 abstract "Abstract In this study, we propose a new algorithm for estimating the annual maximum mixed layer depth (M 2 LD) analogous to a full range of local “ventilation” depth, and corresponding to the deepest surface to which atmospheric influence can be “felt.” Two “seasonality indices” are defined, respectively, for temperature and salinity through Fourier analysis of their time series using Argo data, on the basis of which a significant local minimum of the index corresponding to a maximum penetration depth can be identified. A final M 2 LD is then determined by maximizing the thermal and haline effects. Unlike most of the previous schemes which use arbitrary thresholds or subjective criteria, the new algorithm is objective, robust, and property adaptive provided a significant periodic geophysical forcing such as annual cycle is available. The validity of our methodology is confirmed by the spatial correlation of the tropical dominance of saline effect (mainly related to rainfall cycle) and the extratropical dominance of thermal effect (mainly related to solar cycle). It is also recognized that the M 2 LD distribution is characterized by the coexistence of basin‐scale zonal structures and eddy‐scale local patches. In addition to the fundamental buoyancy forcing caused mainly by latitude‐dependent solar radiation, the impressive two‐scale pattern is found to be primarily attributable to (1) large‐wave climate due to extreme winds (large scale) and (2) systematic eddy shedding as a result of persistent winds (mesoscale). Moreover, a general geographical consistency and a good quantitative agreement are found between the new algorithm and those published in the literature. However, a major discrepancy in our result is the existence of a constantly deeper M 2 LD band compared with other results in the midlatitude oceans of both hemispheres. Given the better correspondence of our M 2 LDs with the depth of the oxygen saturation limit, it is argued that there might be a systematic underestimation with existing criteria in these regions. Our results demonstrate that the M 2 LD may serve as an integrated proxy for studying the coherent multidisciplinary variabilities of the coupled ocean–atmosphere system." @default.
• W2074440415 created "2016-06-24" @default.
• W2074440415 creator A5026498644 @default.
• W2074440415 creator A5076563395 @default.
• W2074440415 date "2015-01-01" @default.
• W2074440415 modified "2023-10-14" @default.
• W2074440415 title "An objective algorithm for estimating maximum oceanic mixed layer depth using seasonality indices derived from <scp>A</scp> rgo temperature/salinity profiles" @default.
• W2074440415 cites W1598462693 @default.
• W2074440415 cites W1967670310 @default.
• W2074440415 cites W1986231519 @default.
• W2074440415 cites W1986498291 @default.
• W2074440415 cites W1997702663 @default.
• W2074440415 cites W1998692757 @default.
• W2074440415 cites W2007398168 @default.
• W2074440415 cites W2008818662 @default.
• W2074440415 cites W2011810038 @default.
• W2074440415 cites W2013686371 @default.
• W2074440415 cites W2016394589 @default.
• W2074440415 cites W2017647804 @default.
• W2074440415 cites W2025371478 @default.
• W2074440415 cites W2030350906 @default.
• W2074440415 cites W2033148357 @default.
• W2074440415 cites W2036480322 @default.
• W2074440415 cites W2042441190 @default.
• W2074440415 cites W2044971647 @default.
• W2074440415 cites W2046883964 @default.
• W2074440415 cites W2052004608 @default.
• W2074440415 cites W2053110663 @default.
• W2074440415 cites W2062384046 @default.
• W2074440415 cites W2066319585 @default.
• W2074440415 cites W2069197937 @default.
• W2074440415 cites W2081999581 @default.
• W2074440415 cites W2082281341 @default.
• W2074440415 cites W2085077672 @default.
• W2074440415 cites W2086829176 @default.
• W2074440415 cites W2088593102 @default.
• W2074440415 cites W2094892216 @default.
• W2074440415 cites W2102482196 @default.
• W2074440415 cites W2103657140 @default.
• W2074440415 cites W2110534741 @default.
• W2074440415 cites W2113186449 @default.
• W2074440415 cites W2115551972 @default.
• W2074440415 cites W2118648278 @default.
• W2074440415 cites W2121179768 @default.
• W2074440415 cites W2166824307 @default.
• W2074440415 cites W2176191286 @default.
• W2074440415 doi "https://doi.org/10.1002/2014jc010383" @default.
• W2074440415 hasPublicationYear "2015" @default.
• W2074440415 type Work @default.
• W2074440415 sameAs 2074440415 @default.
• W2074440415 citedByCount "10" @default.
• W2074440415 countsByYear W20744404152015 @default.
• W2074440415 countsByYear W20744404152016 @default.
• W2074440415 countsByYear W20744404152017 @default.
• W2074440415 countsByYear W20744404152018 @default.
• W2074440415 countsByYear W20744404152019 @default.
• W2074440415 countsByYear W20744404152023 @default.
• W2074440415 crossrefType "journal-article" @default.
• W2074440415 hasAuthorship W2074440415A5026498644 @default.
• W2074440415 hasAuthorship W2074440415A5076563395 @default.
• W2074440415 hasBestOaLocation W20744404151 @default.
• W2074440415 hasConcept C122120755 @default.
• W2074440415 hasConcept C122523270 @default.
• W2074440415 hasConcept C127313418 @default.
• W2074440415 hasConcept C13280743 @default.
• W2074440415 hasConcept C39432304 @default.
• W2074440415 hasConcept C49204034 @default.
• W2074440415 hasConcept C51614570 @default.
• W2074440415 hasConcept C91586092 @default.
• W2074440415 hasConceptScore W2074440415C122120755 @default.
• W2074440415 hasConceptScore W2074440415C122523270 @default.
• W2074440415 hasConceptScore W2074440415C127313418 @default.
• W2074440415 hasConceptScore W2074440415C13280743 @default.
• W2074440415 hasConceptScore W2074440415C39432304 @default.
• W2074440415 hasConceptScore W2074440415C49204034 @default.
• W2074440415 hasConceptScore W2074440415C51614570 @default.
• W2074440415 hasConceptScore W2074440415C91586092 @default.
• W2074440415 hasFunder F4320321001 @default.
• W2074440415 hasFunder F4320327927 @default.
• W2074440415 hasIssue "1" @default.
• W2074440415 hasLocation W20744404151 @default.
• W2074440415 hasOpenAccess W2074440415 @default.
• W2074440415 hasPrimaryLocation W20744404151 @default.
• W2074440415 hasRelatedWork W2008155138 @default.
• W2074440415 hasRelatedWork W2011369223 @default.
• W2074440415 hasRelatedWork W2024936502 @default.
• W2074440415 hasRelatedWork W2082281341 @default.
• W2074440415 hasRelatedWork W2085077672 @default.
• W2074440415 hasRelatedWork W2088166486 @default.
• W2074440415 hasRelatedWork W2093724964 @default.
• W2074440415 hasRelatedWork W2188351259 @default.
• W2074440415 hasRelatedWork W2282259730 @default.
• W2074440415 hasRelatedWork W2784694016 @default.
• W2074440415 hasVolume "120" @default.
• W2074440415 isParatext "false" @default.
• W2074440415 isRetracted "false" @default.
• W2074440415 magId "2074440415" @default.
• W2074440415 workType "article" @default.