FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3139478481> ?p ?o ?g. }

• W3139478481 abstract "Submesoscale circulations influence momentum, buoyancy and transport of biological tracers and pollutants within the upper turbulent layer. How much and how far into the water column this influence extends remain open questions in most of the global ocean. This work evaluates the behavior of neutrally buoyant particles advected in simulations of the northern Gulf of Mexico by analyzing the trajectories of Lagrangian particles released multiple times at the ocean surface and below the mixed layer. The relative role of meso- and submesoscale dynamics is quantified by comparing results in submesoscale permitting and mesoscale resolving simulations. Submesoscale circulations are responsible for greater vertical transport across fixed depth ranges and also across the mixed layer, both into it and away from it, in all seasons. The significance of the submesoscale-induced transport, however, is far greater in winter. In this season, a kernel density estimation and a detailed vertical mixing analysis are performed. It is found that in the large mesoscale Loop Current eddy, upwelling into the mixed layer is the major contributor to the vertical fluxes, despite its clockwise circulation. This is opposite to the behavior simulated in the mesoscale resolving case. In the “submesoscale soup,” away from the large mesoscale structures such as the Loop Current and its detached eddies, upwelling into the mixed layer is distributed more uniformly than downwelling motions from the surface across the base of the mixed layer. Maps of vertical diffusivity indicate that there is an order of magnitude difference among simulations. In the submesoscale permitting case values are distributed around 10 –3 m 2 s –1 in the upper water column in winter, in agreement with recent indirect estimates off the Chilean coast. Diffusivities are greater in the eastern portion of the Gulf, where the submesoscale circulations are more intense due to sustained density gradients supplied by the warmer and saltier Loop Current." @default.
• W3139478481 created "2021-03-29" @default.
• W3139478481 creator A5053680444 @default.
• W3139478481 creator A5073045368 @default.
• W3139478481 creator A5083851252 @default.
• W3139478481 date "2021-03-12" @default.
• W3139478481 modified "2023-10-09" @default.
• W3139478481 title "Submesoscale Mixing Across the Mixed Layer in the Gulf of Mexico" @default.
• W3139478481 cites W1500850684 @default.
• W3139478481 cites W1529149187 @default.
• W3139478481 cites W1749046535 @default.
• W3139478481 cites W1869443795 @default.
• W3139478481 cites W1907224305 @default.
• W3139478481 cites W1963549306 @default.
• W3139478481 cites W1965619916 @default.
• W3139478481 cites W1976439999 @default.
• W3139478481 cites W1979204798 @default.
• W3139478481 cites W1983392676 @default.
• W3139478481 cites W1991869233 @default.
• W3139478481 cites W1994241858 @default.
• W3139478481 cites W2023534137 @default.
• W3139478481 cites W2025346041 @default.
• W3139478481 cites W2029786043 @default.
• W3139478481 cites W2037935425 @default.
• W3139478481 cites W2049103995 @default.
• W3139478481 cites W2052922205 @default.
• W3139478481 cites W2061413830 @default.
• W3139478481 cites W2072166507 @default.
• W3139478481 cites W2076177828 @default.
• W3139478481 cites W2078870438 @default.
• W3139478481 cites W2089027212 @default.
• W3139478481 cites W2090949218 @default.
• W3139478481 cites W2091533595 @default.
• W3139478481 cites W2098334756 @default.
• W3139478481 cites W2100986500 @default.
• W3139478481 cites W2104551033 @default.
• W3139478481 cites W2115830792 @default.
• W3139478481 cites W2121086126 @default.
• W3139478481 cites W2123289934 @default.
• W3139478481 cites W2123786602 @default.
• W3139478481 cites W2125057485 @default.
• W3139478481 cites W2125245236 @default.
• W3139478481 cites W2126533564 @default.
• W3139478481 cites W2135008242 @default.
• W3139478481 cites W2135697520 @default.
• W3139478481 cites W2141125904 @default.
• W3139478481 cites W2148497295 @default.
• W3139478481 cites W2162574928 @default.
• W3139478481 cites W225017691 @default.
• W3139478481 cites W2256337651 @default.
• W3139478481 cites W2276682447 @default.
• W3139478481 cites W2342441820 @default.
• W3139478481 cites W2346337482 @default.
• W3139478481 cites W2372456297 @default.
• W3139478481 cites W2398218541 @default.
• W3139478481 cites W2400488166 @default.
• W3139478481 cites W2592951854 @default.
• W3139478481 cites W2666102564 @default.
• W3139478481 cites W2737505485 @default.
• W3139478481 cites W2739331209 @default.
• W3139478481 cites W2769483327 @default.
• W3139478481 cites W2771523235 @default.
• W3139478481 cites W2794112786 @default.
• W3139478481 cites W2802607877 @default.
• W3139478481 cites W2900064250 @default.
• W3139478481 cites W2942168307 @default.
• W3139478481 cites W2953527216 @default.
• W3139478481 cites W3009580897 @default.
• W3139478481 cites W3014144645 @default.
• W3139478481 cites W3015430112 @default.
• W3139478481 cites W3105206556 @default.
• W3139478481 doi "https://doi.org/10.3389/fmars.2021.615066" @default.
• W3139478481 hasPublicationYear "2021" @default.
• W3139478481 type Work @default.
• W3139478481 sameAs 3139478481 @default.
• W3139478481 citedByCount "10" @default.
• W3139478481 countsByYear W31394784812022 @default.
• W3139478481 countsByYear W31394784812023 @default.
• W3139478481 crossrefType "journal-article" @default.
• W3139478481 hasAuthorship W3139478481A5053680444 @default.
• W3139478481 hasAuthorship W3139478481A5073045368 @default.
• W3139478481 hasAuthorship W3139478481A5083851252 @default.
• W3139478481 hasBestOaLocation W31394784811 @default.
• W3139478481 hasConcept C108699882 @default.
• W3139478481 hasConcept C111368507 @default.
• W3139478481 hasConcept C119601563 @default.
• W3139478481 hasConcept C121332964 @default.
• W3139478481 hasConcept C122120755 @default.
• W3139478481 hasConcept C122846477 @default.
• W3139478481 hasConcept C127313418 @default.
• W3139478481 hasConcept C138777275 @default.
• W3139478481 hasConcept C149348798 @default.
• W3139478481 hasConcept C153294291 @default.
• W3139478481 hasConcept C179065325 @default.
• W3139478481 hasConcept C196558001 @default.
• W3139478481 hasConcept C205649164 @default.
• W3139478481 hasConcept C40382383 @default.
• W3139478481 hasConcept C49204034 @default.
• W3139478481 hasConcept C538625479 @default.
• W3139478481 hasConcept C57879066 @default.

• next