FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2256337651> ?p ?o ?g. }

• W2256337651 endingPage "58" @default.
• W2256337651 startingPage "43" @default.
• W2256337651 abstract "This study examines the mesoscale and submesoscale circulations along the continental slope in the northern Gulf of Mexico at depths greater than 1000 m. The investigation is performed using a regional model run at two horizontal grid resolutions, 5 km and 1.6 km, over a three year period from January 2010 to December 2012. Ageostrophic submesoscale eddies, and vorticity filaments populate the continental slope, and they are stronger and more abundant in the simulation at higher resolution, as to be expected. They are formed from horizontal shear layers at the edges of highly intermittent, bottom-intensified, along-slope boundary currents and in the cores of those currents when they are confined on steep slopes. The horizontal resolution influences the representation of the lateral and vertical transport of neutrally buoyant tracers. This is exemplified by a passive dye deployed near the Macondo Prospect, where the Deepwater Horizon rig exploded in 2010, and at the largest known natural hydrocarbon seep in the northern Gulf, few hundred kilometers to the west of the rig wellhead. The first site is characterized by weak mean currents and, in the high resolution run, by intense submesoscale eddies that form to the west of the Macondo Prospect. GC600, on the other hand, is surrounded by a complicated bathymetry, and its flow is highly variable. The trapping exerted by the submesoscale eddies and vorticity filaments near the rig constrain the spreading in the vicinity of the Macondo Prospect, and as a result, patchiness in the passive tracer distributions differs in the two integrations, despite similar diffusivities expressing the average spreading rate. The tracer released at GC600, on the other hand, is dispersed more effectively in the first six months in the higher resolution case due to enhanced near-bottom turbulent mixing." @default.
• W2256337651 created "2016-06-24" @default.
• W2256337651 creator A5002202304 @default.
• W2256337651 creator A5018257269 @default.
• W2256337651 creator A5049069215 @default.
• W2256337651 creator A5061786786 @default.
• W2256337651 creator A5073045368 @default.
• W2256337651 date "2016-05-01" @default.
• W2256337651 modified "2023-10-10" @default.
• W2256337651 title "Submesoscale currents in the northern Gulf of Mexico: Deep phenomena and dispersion over the continental slope" @default.
• W2256337651 cites W1500850684 @default.
• W2256337651 cites W1672230984 @default.
• W2256337651 cites W1891422992 @default.
• W2256337651 cites W1907224305 @default.
• W2256337651 cites W1940650820 @default.
• W2256337651 cites W1963549306 @default.
• W2256337651 cites W1965619916 @default.
• W2256337651 cites W1973849829 @default.
• W2256337651 cites W1978253701 @default.
• W2256337651 cites W1979204798 @default.
• W2256337651 cites W1980534553 @default.
• W2256337651 cites W1981367618 @default.
• W2256337651 cites W1982197867 @default.
• W2256337651 cites W1986254847 @default.
• W2256337651 cites W1990833884 @default.
• W2256337651 cites W1996436448 @default.
• W2256337651 cites W2003167694 @default.
• W2256337651 cites W2006140268 @default.
• W2256337651 cites W2012754562 @default.
• W2256337651 cites W2013507462 @default.
• W2256337651 cites W2014780309 @default.
• W2256337651 cites W2018431887 @default.
• W2256337651 cites W2020934441 @default.
• W2256337651 cites W2022777787 @default.
• W2256337651 cites W2024638876 @default.
• W2256337651 cites W2025199519 @default.
• W2256337651 cites W2025994957 @default.
• W2256337651 cites W2032572436 @default.
• W2256337651 cites W2035976062 @default.
• W2256337651 cites W2037935425 @default.
• W2256337651 cites W2045127222 @default.
• W2256337651 cites W2047457751 @default.
• W2256337651 cites W2048467149 @default.
• W2256337651 cites W2052258612 @default.
• W2256337651 cites W2061413830 @default.
• W2256337651 cites W2068601543 @default.
• W2256337651 cites W2069735051 @default.
• W2256337651 cites W2072050649 @default.
• W2256337651 cites W2085217406 @default.
• W2256337651 cites W2085552165 @default.
• W2256337651 cites W2087799679 @default.
• W2256337651 cites W2089455804 @default.
• W2256337651 cites W2091533595 @default.
• W2256337651 cites W2110952093 @default.
• W2256337651 cites W2112647302 @default.
• W2256337651 cites W2112829737 @default.
• W2256337651 cites W2116787125 @default.
• W2256337651 cites W2120429925 @default.
• W2256337651 cites W2121745948 @default.
• W2256337651 cites W2125245236 @default.
• W2256337651 cites W2126533564 @default.
• W2256337651 cites W2128254052 @default.
• W2256337651 cites W2134213743 @default.
• W2256337651 cites W2143902752 @default.
• W2256337651 cites W2144046917 @default.
• W2256337651 cites W2148497295 @default.
• W2256337651 cites W2155593826 @default.
• W2256337651 cites W2157409796 @default.
• W2256337651 cites W2166485214 @default.
• W2256337651 cites W2167500235 @default.
• W2256337651 cites W2170684449 @default.
• W2256337651 cites W2171466525 @default.
• W2256337651 cites W2172563153 @default.
• W2256337651 cites W2177598916 @default.
• W2256337651 cites W2179351553 @default.
• W2256337651 cites W2294676268 @default.
• W2256337651 cites W2326923989 @default.
• W2256337651 cites W3102626400 @default.
• W2256337651 doi "https://doi.org/10.1016/j.ocemod.2016.03.002" @default.
• W2256337651 hasPublicationYear "2016" @default.
• W2256337651 type Work @default.
• W2256337651 sameAs 2256337651 @default.
• W2256337651 citedByCount "44" @default.
• W2256337651 countsByYear W22563376512016 @default.
• W2256337651 countsByYear W22563376512017 @default.
• W2256337651 countsByYear W22563376512018 @default.
• W2256337651 countsByYear W22563376512019 @default.
• W2256337651 countsByYear W22563376512020 @default.
• W2256337651 countsByYear W22563376512021 @default.
• W2256337651 countsByYear W22563376512022 @default.
• W2256337651 countsByYear W22563376512023 @default.
• W2256337651 crossrefType "journal-article" @default.
• W2256337651 hasAuthorship W2256337651A5002202304 @default.
• W2256337651 hasAuthorship W2256337651A5018257269 @default.
• W2256337651 hasAuthorship W2256337651A5049069215 @default.
• W2256337651 hasAuthorship W2256337651A5061786786 @default.
• W2256337651 hasAuthorship W2256337651A5073045368 @default.
• W2256337651 hasBestOaLocation W22563376511 @default.

• next