FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2013906064> ?p ?o ?g. }

• W2013906064 endingPage "2030" @default.
• W2013906064 startingPage "2017" @default.
• W2013906064 abstract "El Niño/Southern Oscillation (ENSO)-related patterns of monthly reanalyzed upper-level circulation data and monthly rainfall time series over South America are revised for the 1948–1999 period considering the phases of the Pacific inter-Decadal Oscillation (PDO). The El Niño (EN) related composites show differences relative to the PDO phases as well as seasonal differences. EN signals in the South American rainfall are more conspicuous for the warm PDO (WPDO) regime, when seasonal differences are more pronounced, than for the cold PDO (CPDO). Differences for the 200-hPa stream function composites seem to determine the precipitation composite differences. In fact, the negative precipitation anomalies over northeast Brazil and the excessive rainfall to the south are explained respectively by a cyclonic center over eastern and northeastern Brazil and a weak anticyclonic center over southeastern South America for the WPDO regime. Positive precipitation anomalies over southeastern South America are located in a southern position for the CPDO regime when compared to those for the WPDO regime. These anomalies might be related to a strengthened upper-level subtropical jet stream associated with strong cyclonic circulation extending over southern South America for the CPDO regime. With regard to the linear and nonlinear parts of the precipitation anomaly patterns related to the ENSO, the nonlinear component is considerably smaller than the linear component, in particular, over northern and southeastern South America. This suggests that the linear approach of the South American precipitation response to the ENSO seems to be appropriated. Copyright © 2005 Royal Meteorological Society." @default.
• W2013906064 created "2016-06-24" @default.
• W2013906064 creator A5005893060 @default.
• W2013906064 creator A5053604911 @default.
• W2013906064 date "2005-01-01" @default.
• W2013906064 modified "2023-10-11" @default.
• W2013906064 title "ENSO-related rainfall anomalies in South America and associated circulation features during warm and cold Pacific decadal oscillation regimes" @default.
• W2013906064 cites W1211260759 @default.
• W2013906064 cites W1969357558 @default.
• W2013906064 cites W1993196883 @default.
• W2013906064 cites W2005019103 @default.
• W2013906064 cites W2007077451 @default.
• W2013906064 cites W2014403973 @default.
• W2013906064 cites W2014660626 @default.
• W2013906064 cites W2027461710 @default.
• W2013906064 cites W2038041773 @default.
• W2013906064 cites W2068701783 @default.
• W2013906064 cites W2073077593 @default.
• W2013906064 cites W2083178128 @default.
• W2013906064 cites W2092497323 @default.
• W2013906064 cites W2093401535 @default.
• W2013906064 cites W2099252433 @default.
• W2013906064 cites W2099831531 @default.
• W2013906064 cites W2106459777 @default.
• W2013906064 cites W2107264128 @default.
• W2013906064 cites W2108292794 @default.
• W2013906064 cites W2137582471 @default.
• W2013906064 cites W2142752455 @default.
• W2013906064 cites W2152208495 @default.
• W2013906064 cites W2156412040 @default.
• W2013906064 cites W2173251738 @default.
• W2013906064 cites W2174024865 @default.
• W2013906064 cites W2175179843 @default.
• W2013906064 cites W2178553074 @default.
• W2013906064 cites W2179285547 @default.
• W2013906064 cites W2180555761 @default.
• W2013906064 cites W2180602820 @default.
• W2013906064 cites W2180640486 @default.
• W2013906064 cites W4254654104 @default.
• W2013906064 doi "https://doi.org/10.1002/joc.1222" @default.
• W2013906064 hasPublicationYear "2005" @default.
• W2013906064 type Work @default.
• W2013906064 sameAs 2013906064 @default.
• W2013906064 citedByCount "178" @default.
• W2013906064 countsByYear W20139060642012 @default.
• W2013906064 countsByYear W20139060642013 @default.
• W2013906064 countsByYear W20139060642014 @default.
• W2013906064 countsByYear W20139060642015 @default.
• W2013906064 countsByYear W20139060642016 @default.
• W2013906064 countsByYear W20139060642017 @default.
• W2013906064 countsByYear W20139060642018 @default.
• W2013906064 countsByYear W20139060642019 @default.
• W2013906064 countsByYear W20139060642020 @default.
• W2013906064 countsByYear W20139060642021 @default.
• W2013906064 countsByYear W20139060642022 @default.
• W2013906064 countsByYear W20139060642023 @default.
• W2013906064 crossrefType "journal-article" @default.
• W2013906064 hasAuthorship W2013906064A5005893060 @default.
• W2013906064 hasAuthorship W2013906064A5053604911 @default.
• W2013906064 hasBestOaLocation W20139060641 @default.
• W2013906064 hasConcept C107054158 @default.
• W2013906064 hasConcept C119947313 @default.
• W2013906064 hasConcept C121332964 @default.
• W2013906064 hasConcept C127313418 @default.
• W2013906064 hasConcept C12997251 @default.
• W2013906064 hasConcept C14168384 @default.
• W2013906064 hasConcept C150284090 @default.
• W2013906064 hasConcept C153294291 @default.
• W2013906064 hasConcept C154808844 @default.
• W2013906064 hasConcept C160945548 @default.
• W2013906064 hasConcept C162164538 @default.
• W2013906064 hasConcept C205649164 @default.
• W2013906064 hasConcept C26873012 @default.
• W2013906064 hasConcept C39432304 @default.
• W2013906064 hasConcept C49204034 @default.
• W2013906064 hasConcept C505870484 @default.
• W2013906064 hasConcept C507956050 @default.
• W2013906064 hasConcept C51040755 @default.
• W2013906064 hasConcept C67320510 @default.
• W2013906064 hasConcept C86803240 @default.
• W2013906064 hasConcept C97355855 @default.
• W2013906064 hasConceptScore W2013906064C107054158 @default.
• W2013906064 hasConceptScore W2013906064C119947313 @default.
• W2013906064 hasConceptScore W2013906064C121332964 @default.
• W2013906064 hasConceptScore W2013906064C127313418 @default.
• W2013906064 hasConceptScore W2013906064C12997251 @default.
• W2013906064 hasConceptScore W2013906064C14168384 @default.
• W2013906064 hasConceptScore W2013906064C150284090 @default.
• W2013906064 hasConceptScore W2013906064C153294291 @default.
• W2013906064 hasConceptScore W2013906064C154808844 @default.
• W2013906064 hasConceptScore W2013906064C160945548 @default.
• W2013906064 hasConceptScore W2013906064C162164538 @default.
• W2013906064 hasConceptScore W2013906064C205649164 @default.
• W2013906064 hasConceptScore W2013906064C26873012 @default.
• W2013906064 hasConceptScore W2013906064C39432304 @default.
• W2013906064 hasConceptScore W2013906064C49204034 @default.
• W2013906064 hasConceptScore W2013906064C505870484 @default.
• W2013906064 hasConceptScore W2013906064C507956050 @default.

• next