FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2074702965> ?p ?o ?g. }

• W2074702965 endingPage "3040" @default.
• W2074702965 startingPage "3033" @default.
• W2074702965 abstract "A composite NOAA 14 satellite advanced very high resolution radiometer image of the Gulf of Alaska for early March 1995 reveals a sequence of six anticyclonic oceanic eddies spanning more than 1500 km of the continental margin of North America from central British Columbia to central Alaska. Although isolated mesoscale eddies have previously been documented for this eastern boundary region, the composite image provides the first evidence that trains of such eddies can develop “simultaneously” along the entire coast. The 80 km radius and 250 km spacing of these warm‐core eddies are consistent with a baroclinic instability event in the poleward coastal current that prevails along the northwest continental margin of North America in “winter” (roughly October through March). Wind data from offshore meteorological buoys, combined with partial cloud‐free thermal images for January and February, suggest that the event was triggered in mid January by an abrupt, coast‐wide reversal in the prevailing poleward wind. The instability event disrupted the alongshore transport of relatively warm, high‐salinity water and presumably resulted in a greatly enhanced cross‐shore flux of brackish, nutrient‐rich coastal water into the open ocean. On the basis of its basin‐scale extent and more than 2 month duration it is feasible that the event had a major impact on the early spring recruitment and survival of zooplankton and pelagic fish within the highly productive fishery zones of coastal British Columbia and Alaska. Less extensive eddy sequences found in several earlier satellite images for the region suggest that these instability events are fairly common. If so, this indicates that the poleward current that forms over the eastern Pacific continental slope in late fall (herein, the “Northeast Pacific Coastal Current”) is marginally stable and likely to deform into a series of mesoscale eddies following abrupt, basin‐scale reversals in the seasonally dominant wind. Provided these wind events occur early enough in the season, the coastal current could reform with the onset of poleward winter winds." @default.
• W2074702965 created "2016-06-24" @default.
• W2074702965 creator A5032155956 @default.
• W2074702965 creator A5085041281 @default.
• W2074702965 date "1998-02-15" @default.
• W2074702965 modified "2023-09-26" @default.
• W2074702965 title "A basin-scale oceanic instability event in the Gulf of Alaska" @default.
• W2074702965 cites W1160649415 @default.
• W2074702965 cites W1485205350 @default.
• W2074702965 cites W1966543639 @default.
• W2074702965 cites W1986033755 @default.
• W2074702965 cites W1988168137 @default.
• W2074702965 cites W1988399945 @default.
• W2074702965 cites W1990480127 @default.
• W2074702965 cites W1997505678 @default.
• W2074702965 cites W1998036329 @default.
• W2074702965 cites W2002623542 @default.
• W2074702965 cites W2011288877 @default.
• W2074702965 cites W2018957117 @default.
• W2074702965 cites W2023091514 @default.
• W2074702965 cites W2043796348 @default.
• W2074702965 cites W2050208411 @default.
• W2074702965 cites W2057757382 @default.
• W2074702965 cites W2065758300 @default.
• W2074702965 cites W2083056192 @default.
• W2074702965 cites W2091038058 @default.
• W2074702965 cites W2093024520 @default.
• W2074702965 cites W2093959506 @default.
• W2074702965 cites W322670869 @default.
• W2074702965 cites W2132865881 @default.
• W2074702965 doi "https://doi.org/10.1029/97jc03220" @default.
• W2074702965 hasPublicationYear "1998" @default.
• W2074702965 type Work @default.
• W2074702965 sameAs 2074702965 @default.
• W2074702965 citedByCount "99" @default.
• W2074702965 countsByYear W20747029652012 @default.
• W2074702965 countsByYear W20747029652013 @default.
• W2074702965 countsByYear W20747029652014 @default.
• W2074702965 countsByYear W20747029652015 @default.
• W2074702965 countsByYear W20747029652016 @default.
• W2074702965 countsByYear W20747029652018 @default.
• W2074702965 countsByYear W20747029652021 @default.
• W2074702965 countsByYear W20747029652022 @default.
• W2074702965 countsByYear W20747029652023 @default.
• W2074702965 crossrefType "journal-article" @default.
• W2074702965 hasAuthorship W2074702965A5032155956 @default.
• W2074702965 hasAuthorship W2074702965A5085041281 @default.
• W2074702965 hasConcept C109007969 @default.
• W2074702965 hasConcept C111368507 @default.
• W2074702965 hasConcept C127313418 @default.
• W2074702965 hasConcept C151730666 @default.
• W2074702965 hasConcept C153294291 @default.
• W2074702965 hasConcept C179065325 @default.
• W2074702965 hasConcept C184751465 @default.
• W2074702965 hasConcept C187599188 @default.
• W2074702965 hasConcept C196558001 @default.
• W2074702965 hasConcept C20364790 @default.
• W2074702965 hasConcept C205649164 @default.
• W2074702965 hasConcept C49204034 @default.
• W2074702965 hasConcept C53631411 @default.
• W2074702965 hasConcept C60069189 @default.
• W2074702965 hasConcept C67320510 @default.
• W2074702965 hasConceptScore W2074702965C109007969 @default.
• W2074702965 hasConceptScore W2074702965C111368507 @default.
• W2074702965 hasConceptScore W2074702965C127313418 @default.
• W2074702965 hasConceptScore W2074702965C151730666 @default.
• W2074702965 hasConceptScore W2074702965C153294291 @default.
• W2074702965 hasConceptScore W2074702965C179065325 @default.
• W2074702965 hasConceptScore W2074702965C184751465 @default.
• W2074702965 hasConceptScore W2074702965C187599188 @default.
• W2074702965 hasConceptScore W2074702965C196558001 @default.
• W2074702965 hasConceptScore W2074702965C20364790 @default.
• W2074702965 hasConceptScore W2074702965C205649164 @default.
• W2074702965 hasConceptScore W2074702965C49204034 @default.
• W2074702965 hasConceptScore W2074702965C53631411 @default.
• W2074702965 hasConceptScore W2074702965C60069189 @default.
• W2074702965 hasConceptScore W2074702965C67320510 @default.
• W2074702965 hasIssue "C2" @default.
• W2074702965 hasLocation W20747029651 @default.
• W2074702965 hasOpenAccess W2074702965 @default.
• W2074702965 hasPrimaryLocation W20747029651 @default.
• W2074702965 hasRelatedWork W1489182398 @default.
• W2074702965 hasRelatedWork W1994594946 @default.
• W2074702965 hasRelatedWork W2025140260 @default.
• W2074702965 hasRelatedWork W2064193917 @default.
• W2074702965 hasRelatedWork W2064428790 @default.
• W2074702965 hasRelatedWork W2176882698 @default.
• W2074702965 hasRelatedWork W2921251871 @default.
• W2074702965 hasRelatedWork W4212782278 @default.
• W2074702965 hasRelatedWork W4311903923 @default.
• W2074702965 hasRelatedWork W249478361 @default.
• W2074702965 hasVolume "103" @default.
• W2074702965 isParatext "false" @default.
• W2074702965 isRetracted "false" @default.
• W2074702965 magId "2074702965" @default.
• W2074702965 workType "article" @default.