FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1977524900> ?p ?o ?g. }

• W1977524900 endingPage "10817" @default.
• W1977524900 startingPage "10817" @default.
• W1977524900 abstract "The two principal fronts within the Antarctic Circumpolar Current (ACC), the Subantarctic Front (SAF) and the Polar Front (PF), are investigated with respect to their spatial patterns and relations to deep water masses from the northern Drake Passage to the western and southern Argentine Basin. Observations from four recent cruises in adjoining and overlapping regions are supplemented with satellite infrared imagery and trajectories from surface drifters. East of Drake Passage, the width of the Polar Frontal Zone (PFZ) increases rapidly when the SAF turns sharply northward as a part of the Falkland (Malvinas) Current, while the PF remains oriented mainly toward the northeast. Found within this region of the PFZ are mesoscale eddies, the upper layers of which consist of Subantarctic Mode Water from the Pacific. The contrasts in upper layer water properties that identify the SAF can be traced the entire length of the Falkland Current to the Brazil-Falkland confluence zone and then southward to the southern Argentine Basin. There the SAF turns eastward and later, but perhaps not always, merges with the PF north of Ewing Bank to form a single, intense current core strongly influenced by bottom topography. At times this eastward current loops southward through a gap in the Falkland Ridge into the Georgia Basin, thereby supplying relatively warm and salty Subantarctic water to the Antarctic Zone. East of the gap, the two fronts become separated and are once again distinct features in the vicinity of the Islas Orcadas Rise. At depth, within Drake Passage and the western Scotia Sea, the SAF and PF are not lateral boundaries between distinct water masses, but are instead identified by enhanced vertical displacements of property isopleths. With the northward turn of the SAF east of Drake Passage, a thick layer of Circumpolar Deep Water (CDW) is advected over the Falkland Plateau into the Argentine Basin. There it is joined by waters entering the Argentine Basin via a deep spreading route through the Georgia Basin: denser CDW, deep water from the Weddell Sea, and episodically, deep water from the southeastern Pacific Ocean. Together, these waters form a northward flow off the Patagonian shelf that extends from the sea surface to the bottom, most of which turns back toward the south with the Falkland Current return. Also flowing south, along the seaward side of the Falkland Current return well away from the western boundary, is the main core of North Atlantic Deep Water (NADW). Detatched masses of NADW are observed within the CDW at the western boundary as well as within the ACC south of the SAF in the south central Argentine Basin." @default.
• W1977524900 created "2016-06-24" @default.
• W1977524900 creator A5053892345 @default.
• W1977524900 creator A5066559442 @default.
• W1977524900 date "1989-01-01" @default.
• W1977524900 modified "2023-10-14" @default.
• W1977524900 title "The subantarctic and polar fronts in relation to deep water masses through the southwestern Atlantic" @default.
• W1977524900 cites W1965219285 @default.
• W1977524900 cites W1969529205 @default.
• W1977524900 cites W1970136052 @default.
• W1977524900 cites W1982834334 @default.
• W1977524900 cites W1986511731 @default.
• W1977524900 cites W1989630370 @default.
• W1977524900 cites W1996673372 @default.
• W1977524900 cites W2005662711 @default.
• W1977524900 cites W2014954478 @default.
• W1977524900 cites W2015720815 @default.
• W1977524900 cites W2019362864 @default.
• W1977524900 cites W2023042176 @default.
• W1977524900 cites W2030043136 @default.
• W1977524900 cites W2030488308 @default.
• W1977524900 cites W2034066382 @default.
• W1977524900 cites W2034504801 @default.
• W1977524900 cites W2034550525 @default.
• W1977524900 cites W2042408465 @default.
• W1977524900 cites W2043954881 @default.
• W1977524900 cites W2061109775 @default.
• W1977524900 cites W2062480296 @default.
• W1977524900 cites W2066805998 @default.
• W1977524900 cites W2087020531 @default.
• W1977524900 cites W2088826953 @default.
• W1977524900 cites W2155190463 @default.
• W1977524900 doi "https://doi.org/10.1029/jc094ic08p10817" @default.
• W1977524900 hasPublicationYear "1989" @default.
• W1977524900 type Work @default.
• W1977524900 sameAs 1977524900 @default.
• W1977524900 citedByCount "232" @default.
• W1977524900 countsByYear W19775249002012 @default.
• W1977524900 countsByYear W19775249002013 @default.
• W1977524900 countsByYear W19775249002014 @default.
• W1977524900 countsByYear W19775249002015 @default.
• W1977524900 countsByYear W19775249002016 @default.
• W1977524900 countsByYear W19775249002017 @default.
• W1977524900 countsByYear W19775249002018 @default.
• W1977524900 countsByYear W19775249002019 @default.
• W1977524900 countsByYear W19775249002020 @default.
• W1977524900 countsByYear W19775249002021 @default.
• W1977524900 countsByYear W19775249002022 @default.
• W1977524900 countsByYear W19775249002023 @default.
• W1977524900 crossrefType "journal-article" @default.
• W1977524900 hasAuthorship W1977524900A5053892345 @default.
• W1977524900 hasAuthorship W1977524900A5066559442 @default.
• W1977524900 hasBestOaLocation W19775249002 @default.
• W1977524900 hasConcept C111368507 @default.
• W1977524900 hasConcept C121332964 @default.
• W1977524900 hasConcept C127313418 @default.
• W1977524900 hasConcept C1276947 @default.
• W1977524900 hasConcept C140302290 @default.
• W1977524900 hasConcept C157485413 @default.
• W1977524900 hasConcept C25343380 @default.
• W1977524900 hasConcept C2777551076 @default.
• W1977524900 hasConcept C29705727 @default.
• W1977524900 hasConcept C2988134249 @default.
• W1977524900 hasConcept C41008148 @default.
• W1977524900 hasConcept C6582778 @default.
• W1977524900 hasConcept C77088390 @default.
• W1977524900 hasConcept C83133772 @default.
• W1977524900 hasConceptScore W1977524900C111368507 @default.
• W1977524900 hasConceptScore W1977524900C121332964 @default.
• W1977524900 hasConceptScore W1977524900C127313418 @default.
• W1977524900 hasConceptScore W1977524900C1276947 @default.
• W1977524900 hasConceptScore W1977524900C140302290 @default.
• W1977524900 hasConceptScore W1977524900C157485413 @default.
• W1977524900 hasConceptScore W1977524900C25343380 @default.
• W1977524900 hasConceptScore W1977524900C2777551076 @default.
• W1977524900 hasConceptScore W1977524900C29705727 @default.
• W1977524900 hasConceptScore W1977524900C2988134249 @default.
• W1977524900 hasConceptScore W1977524900C41008148 @default.
• W1977524900 hasConceptScore W1977524900C6582778 @default.
• W1977524900 hasConceptScore W1977524900C77088390 @default.
• W1977524900 hasConceptScore W1977524900C83133772 @default.
• W1977524900 hasIssue "C8" @default.
• W1977524900 hasLocation W19775249001 @default.
• W1977524900 hasLocation W19775249002 @default.
• W1977524900 hasOpenAccess W1977524900 @default.
• W1977524900 hasPrimaryLocation W19775249001 @default.
• W1977524900 hasRelatedWork W1673570755 @default.
• W1977524900 hasRelatedWork W1977524900 @default.
• W1977524900 hasRelatedWork W1993794136 @default.
• W1977524900 hasRelatedWork W2013249079 @default.
• W1977524900 hasRelatedWork W2062480296 @default.
• W1977524900 hasRelatedWork W2068003081 @default.
• W1977524900 hasRelatedWork W2090068314 @default.
• W1977524900 hasRelatedWork W2567698666 @default.
• W1977524900 hasRelatedWork W2725430322 @default.
• W1977524900 hasRelatedWork W4238011843 @default.
• W1977524900 hasVolume "94" @default.
• W1977524900 isParatext "false" @default.

• next