FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2110772710> ?p ?o ?g. }

• W2110772710 endingPage "4321" @default.
• W2110772710 startingPage "4316" @default.
• W2110772710 abstract "Abstract Decadal variations of very small amplitude [∼0.3°C in sea surface temperature (SST)] in the tropical Pacific Ocean, the genesis region of the interannual El Niño–Southern Oscillation (ENSO) phenomenon, have been shown to have powerful impacts on global climate. Future projections from different climate models do not agree on how this critical feature will change under the influence of anthropogenic forcing. A number of attempts have been made to resolve this issue by examining observed trends from the 1880s to the present, a period of rising atmospheric concentrations of greenhouse gases. A recent attempt concluded that the three major datasets disagreed on the trend in the equatorial gradient of SST. Using a corrected version of one of these datasets, and extending the analysis to the seasonal cycle, it is shown here that all agree that the equatorial Pacific zonal SST gradient has strengthened from 1880 to 2005 during the boreal fall when this gradient is normally strongest. This result appears to favor a theory for future changes based on ocean dynamics over one based on atmospheric energy considerations. Both theories incorporate the expectation, based on ENSO theory, that the zonal sea level pressure (SLP) gradient in the tropical Pacific is coupled to SST and should therefore strengthen along with the SST gradient. While the SLP gradient has not strengthened, it is found that it appears to have weakened only during boreal spring, consistent with the SST seasonal trends. Most of the coupled models included in the Intergovernmental Panel on Climate Change (IPCC) Fourth Assessment Report underestimate the strengthening SST gradient in boreal fall, and show almost no change in the SLP gradient in any season. The observational analyses herein suggest that both theories are at work but with relative strengths that vary seasonally, and that the two theories need not be inconsistent with each other." @default.
• W2110772710 created "2016-06-24" @default.
• W2110772710 creator A5000307534 @default.
• W2110772710 creator A5000493164 @default.
• W2110772710 creator A5006085453 @default.
• W2110772710 creator A5007424651 @default.
• W2110772710 creator A5065775518 @default.
• W2110772710 date "2009-08-15" @default.
• W2110772710 modified "2023-10-17" @default.
• W2110772710 title "Observed Strengthening of the Zonal Sea Surface Temperature Gradient across the Equatorial Pacific Ocean*" @default.
• W2110772710 cites W1989272559 @default.
• W2110772710 cites W1999037513 @default.
• W2110772710 cites W2006165291 @default.
• W2110772710 cites W2018764772 @default.
• W2110772710 cites W2023824808 @default.
• W2110772710 cites W2035891155 @default.
• W2110772710 cites W2038451290 @default.
• W2110772710 cites W2052734296 @default.
• W2110772710 cites W2055192091 @default.
• W2110772710 cites W2068413743 @default.
• W2110772710 cites W2072128221 @default.
• W2110772710 cites W2078030647 @default.
• W2110772710 cites W2079753076 @default.
• W2110772710 cites W2091388550 @default.
• W2110772710 cites W2108527489 @default.
• W2110772710 cites W2122511023 @default.
• W2110772710 cites W2123241285 @default.
• W2110772710 cites W2141777143 @default.
• W2110772710 cites W2174279521 @default.
• W2110772710 cites W2174848188 @default.
• W2110772710 cites W2176202464 @default.
• W2110772710 cites W2318680928 @default.
• W2110772710 cites W4256444905 @default.
• W2110772710 doi "https://doi.org/10.1175/2009jcli2936.1" @default.
• W2110772710 hasPublicationYear "2009" @default.
• W2110772710 type Work @default.
• W2110772710 sameAs 2110772710 @default.
• W2110772710 citedByCount "133" @default.
• W2110772710 countsByYear W21107727102012 @default.
• W2110772710 countsByYear W21107727102013 @default.
• W2110772710 countsByYear W21107727102014 @default.
• W2110772710 countsByYear W21107727102015 @default.
• W2110772710 countsByYear W21107727102016 @default.
• W2110772710 countsByYear W21107727102017 @default.
• W2110772710 countsByYear W21107727102018 @default.
• W2110772710 countsByYear W21107727102019 @default.
• W2110772710 countsByYear W21107727102020 @default.
• W2110772710 countsByYear W21107727102021 @default.
• W2110772710 countsByYear W21107727102022 @default.
• W2110772710 countsByYear W21107727102023 @default.
• W2110772710 crossrefType "journal-article" @default.
• W2110772710 hasAuthorship W2110772710A5000307534 @default.
• W2110772710 hasAuthorship W2110772710A5000493164 @default.
• W2110772710 hasAuthorship W2110772710A5006085453 @default.
• W2110772710 hasAuthorship W2110772710A5007424651 @default.
• W2110772710 hasAuthorship W2110772710A5065775518 @default.
• W2110772710 hasBestOaLocation W21107727101 @default.
• W2110772710 hasConcept C100537666 @default.
• W2110772710 hasConcept C111368507 @default.
• W2110772710 hasConcept C115343472 @default.
• W2110772710 hasConcept C127313418 @default.
• W2110772710 hasConcept C132651083 @default.
• W2110772710 hasConcept C134097258 @default.
• W2110772710 hasConcept C137109543 @default.
• W2110772710 hasConcept C151730666 @default.
• W2110772710 hasConcept C153294291 @default.
• W2110772710 hasConcept C154808844 @default.
• W2110772710 hasConcept C168754636 @default.
• W2110772710 hasConcept C197115733 @default.
• W2110772710 hasConcept C205649164 @default.
• W2110772710 hasConcept C39432304 @default.
• W2110772710 hasConcept C49204034 @default.
• W2110772710 hasConcept C507956050 @default.
• W2110772710 hasConcept C91586092 @default.
• W2110772710 hasConceptScore W2110772710C100537666 @default.
• W2110772710 hasConceptScore W2110772710C111368507 @default.
• W2110772710 hasConceptScore W2110772710C115343472 @default.
• W2110772710 hasConceptScore W2110772710C127313418 @default.
• W2110772710 hasConceptScore W2110772710C132651083 @default.
• W2110772710 hasConceptScore W2110772710C134097258 @default.
• W2110772710 hasConceptScore W2110772710C137109543 @default.
• W2110772710 hasConceptScore W2110772710C151730666 @default.
• W2110772710 hasConceptScore W2110772710C153294291 @default.
• W2110772710 hasConceptScore W2110772710C154808844 @default.
• W2110772710 hasConceptScore W2110772710C168754636 @default.
• W2110772710 hasConceptScore W2110772710C197115733 @default.
• W2110772710 hasConceptScore W2110772710C205649164 @default.
• W2110772710 hasConceptScore W2110772710C39432304 @default.
• W2110772710 hasConceptScore W2110772710C49204034 @default.
• W2110772710 hasConceptScore W2110772710C507956050 @default.
• W2110772710 hasConceptScore W2110772710C91586092 @default.
• W2110772710 hasIssue "16" @default.
• W2110772710 hasLocation W21107727101 @default.
• W2110772710 hasOpenAccess W2110772710 @default.
• W2110772710 hasPrimaryLocation W21107727101 @default.
• W2110772710 hasRelatedWork W2105100550 @default.
• W2110772710 hasRelatedWork W2110772710 @default.
• W2110772710 hasRelatedWork W2218367494 @default.

• next