FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2296227534> ?p ?o ?g. }

• W2296227534 endingPage "2181" @default.
• W2296227534 startingPage "2167" @default.
• W2296227534 abstract "Abstract. The temporal evolution of the physical and biogeochemical structure of an oxygen-depleted anticyclonic modewater eddy is investigated over a 2-month period using high-resolution glider and ship data. A weakly stratified eddy core (squared buoyancy frequency N2 ∼ 0.1 × 10−4 s−2) at shallow depth is identified with a horizontal extent of about 70 km and bounded by maxima in N2. The upper N2 maximum (3–5 × 10−4 s−2) coincides with the mixed layer base and the lower N2 maximum (0.4 × 10−4 s−2) is found at about 200 m depth in the eddy centre. The eddy core shows a constant slope in temperature/salinity (T∕S) characteristic over the 2 months, but an erosion of the core progressively narrows down the T∕S range. The eddy minimal oxygen concentrations decreased by about 5 µmol kg−1 in 2 months, confirming earlier estimates of oxygen consumption rates in these eddies. Separating the mesoscale and perturbation flow components reveals oscillating velocity finestructure ( ∼ 0.1 m s−1) underneath the eddy and at its flanks. The velocity finestructure is organized in layers that align with layers in properties (salinity, temperature) but mostly cross through surfaces of constant density. The largest magnitude in velocity finestructure is seen between the surface and 140 m just outside the maximum mesoscale flow but also in a layer underneath the eddy centre, between 250 and 450 m. For both regions a cyclonic rotation of the velocity finestructure with depth suggests the vertical propagation of near-inertial wave (NIW) energy. Modification of the planetary vorticity by anticyclonic (eddy core) and cyclonic (eddy periphery) relative vorticity is most likely impacting the NIW energy propagation. Below the low oxygen core salt-finger type double diffusive layers are found that align with the velocity finestructure. Apparent oxygen utilization (AOU) versus dissolved inorganic nitrate (NO3−) ratios are about twice as high (16) in the eddy core compared to surrounding waters (8.1). A large NO3− deficit of 4 to 6 µmol kg−1 is determined, rendering denitrification an unlikely explanation. Here it is hypothesized that the differences in local recycling of nitrogen and oxygen, as a result of the eddy dynamics, cause the shift in the AOU : NO3− ratio. High NO3− and low oxygen waters are eroded by mixing from the eddy core and entrain into the mixed layer. The nitrogen is reintroduced into the core by gravitational settling of particulate matter out of the euphotic zone. The low oxygen water equilibrates in the mixed layer by air–sea gas exchange and does not participate in the gravitational sinking. Finally we propose a mesoscale–submesoscale interaction concept where wind energy, mediated via NIWs, drives nutrient supply to the euphotic zone and drives extraordinary blooms in anticyclonic mode-water eddies." @default.
• W2296227534 created "2016-06-24" @default.
• W2296227534 creator A5003302071 @default.
• W2296227534 creator A5014068393 @default.
• W2296227534 creator A5015216269 @default.
• W2296227534 creator A5020822826 @default.
• W2296227534 creator A5029064640 @default.
• W2296227534 creator A5038935174 @default.
• W2296227534 creator A5040182971 @default.
• W2296227534 creator A5045501351 @default.
• W2296227534 creator A5051317140 @default.
• W2296227534 creator A5066631224 @default.
• W2296227534 creator A5079453133 @default.
• W2296227534 creator A5088254346 @default.
• W2296227534 date "2017-04-27" @default.
• W2296227534 modified "2023-10-15" @default.
• W2296227534 title "Upwelling and isolation in oxygen-depleted anticyclonic modewater eddies and implications for nitrate cycling" @default.
• W2296227534 cites W1496279843 @default.
• W2296227534 cites W1556096174 @default.
• W2296227534 cites W1570586122 @default.
• W2296227534 cites W157078197 @default.
• W2296227534 cites W1655188195 @default.
• W2296227534 cites W1905874590 @default.
• W2296227534 cites W1907224305 @default.
• W2296227534 cites W1919750483 @default.
• W2296227534 cites W1941403918 @default.
• W2296227534 cites W1970953573 @default.
• W2296227534 cites W1972215191 @default.
• W2296227534 cites W1973926848 @default.
• W2296227534 cites W1981765997 @default.
• W2296227534 cites W1984179025 @default.
• W2296227534 cites W1985682203 @default.
• W2296227534 cites W1989712626 @default.
• W2296227534 cites W2006563928 @default.
• W2296227534 cites W2017647804 @default.
• W2296227534 cites W2020585322 @default.
• W2296227534 cites W2026523672 @default.
• W2296227534 cites W2030653675 @default.
• W2296227534 cites W2049171398 @default.
• W2296227534 cites W2051497614 @default.
• W2296227534 cites W2055107683 @default.
• W2296227534 cites W2059989995 @default.
• W2296227534 cites W2073973319 @default.
• W2296227534 cites W2075403956 @default.
• W2296227534 cites W2078401285 @default.
• W2296227534 cites W2081748947 @default.
• W2296227534 cites W2083524788 @default.
• W2296227534 cites W2088787857 @default.
• W2296227534 cites W2103076838 @default.
• W2296227534 cites W2112736998 @default.
• W2296227534 cites W2145960535 @default.
• W2296227534 cites W2169842902 @default.
• W2296227534 cites W2177482784 @default.
• W2296227534 cites W2196955856 @default.
• W2296227534 cites W2221482649 @default.
• W2296227534 cites W2326107249 @default.
• W2296227534 cites W2400488166 @default.
• W2296227534 cites W2403625973 @default.
• W2296227534 cites W2469914133 @default.
• W2296227534 cites W2544696101 @default.
• W2296227534 cites W2570345203 @default.
• W2296227534 cites W2728252509 @default.
• W2296227534 doi "https://doi.org/10.5194/bg-14-2167-2017" @default.
• W2296227534 hasPublicationYear "2017" @default.
• W2296227534 type Work @default.
• W2296227534 sameAs 2296227534 @default.
• W2296227534 citedByCount "39" @default.
• W2296227534 countsByYear W22962275342017 @default.
• W2296227534 countsByYear W22962275342018 @default.
• W2296227534 countsByYear W22962275342019 @default.
• W2296227534 countsByYear W22962275342020 @default.
• W2296227534 countsByYear W22962275342021 @default.
• W2296227534 countsByYear W22962275342022 @default.
• W2296227534 countsByYear W22962275342023 @default.
• W2296227534 crossrefType "journal-article" @default.
• W2296227534 hasAuthorship W2296227534A5003302071 @default.
• W2296227534 hasAuthorship W2296227534A5014068393 @default.
• W2296227534 hasAuthorship W2296227534A5015216269 @default.
• W2296227534 hasAuthorship W2296227534A5020822826 @default.
• W2296227534 hasAuthorship W2296227534A5029064640 @default.
• W2296227534 hasAuthorship W2296227534A5038935174 @default.
• W2296227534 hasAuthorship W2296227534A5040182971 @default.
• W2296227534 hasAuthorship W2296227534A5045501351 @default.
• W2296227534 hasAuthorship W2296227534A5051317140 @default.
• W2296227534 hasAuthorship W2296227534A5066631224 @default.
• W2296227534 hasAuthorship W2296227534A5079453133 @default.
• W2296227534 hasAuthorship W2296227534A5088254346 @default.
• W2296227534 hasBestOaLocation W22962275341 @default.
• W2296227534 hasConcept C100701293 @default.
• W2296227534 hasConcept C104196234 @default.
• W2296227534 hasConcept C111368507 @default.
• W2296227534 hasConcept C121332964 @default.
• W2296227534 hasConcept C122120755 @default.
• W2296227534 hasConcept C127313418 @default.
• W2296227534 hasConcept C129513315 @default.
• W2296227534 hasConcept C149348798 @default.
• W2296227534 hasConcept C179065325 @default.
• W2296227534 hasConcept C192943249 @default.

• next