FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2938492869> ?p ?o ?g. }

• W2938492869 endingPage "3411" @default.
• W2938492869 startingPage "3396" @default.
• W2938492869 abstract "Abstract The present study investigates the diversity of the La Niña decaying phase and the corresponding spring and summer precipitation anomalies over the eastern China. Based on the differences in sea surface temperature anomaly (SSTA) evolution during the La Niña decaying phase, 18 La Niña events in the period 1961–2016 are classified into three types—namely, the “persistent type” (P‐type), the “re‐intensified type” (R‐type), and the “fast‐decay type” (F‐type). Precipitation responses over eastern China during the decaying spring and summer of the three types of La Niña present significant differences. For the R‐type La Niña decaying spring, the enhanced precipitation appears over northeastern China but significant suppressed precipitation anomalies are observed elsewhere, particularly in Yellow River basin, the Yangtze River basin, and southeastern China. Significant negative precipitation anomaly appears over northeastern China in both P‐type and F‐type La Niña decaying spring. In the decaying summer, for P‐type La Niña, dry anomalies are apparent in southern and northern China. For R‐type La Niña, negative rainfall anomalies are notable in northeastern China, the Hetao region, and the middle reaches of the Yangtze River basin. For F‐type La Niña, significant negative rainfall anomalies are found over the Yangtze River basin and parts of northern China. The responses of the large‐scale circulation anomalies to the distinct SSTA patterns of the different types of La Niña are responsible for the diversity of rainfall anomalies over eastern China. The precipitation anomaly pattern in eastern China is closely associated with the different types of La Niña decay, and it is seasonal‐dependent. These two aspects should be taken into account when conducting seasonal predictions of spring and summer rainfall anomalies over eastern China using El Niño–Southern Oscillation as a predictor." @default.
• W2938492869 created "2019-04-25" @default.
• W2938492869 creator A5000139565 @default.
• W2938492869 creator A5007247287 @default.
• W2938492869 creator A5031805159 @default.
• W2938492869 creator A5047358306 @default.
• W2938492869 creator A5047669781 @default.
• W2938492869 date "2019-04-24" @default.
• W2938492869 modified "2023-10-16" @default.
• W2938492869 title "The diversity of La Niña decay and the corresponding spring and summer precipitation anomalies over eastern China" @default.
• W2938492869 cites W1735671984 @default.
• W2938492869 cites W1851706974 @default.
• W2938492869 cites W1970460217 @default.
• W2938492869 cites W2006165291 @default.
• W2938492869 cites W2008147830 @default.
• W2938492869 cites W2018304142 @default.
• W2938492869 cites W2020952897 @default.
• W2938492869 cites W2023128436 @default.
• W2938492869 cites W2023372691 @default.
• W2938492869 cites W2023875545 @default.
• W2938492869 cites W2028247729 @default.
• W2938492869 cites W2030081190 @default.
• W2938492869 cites W2030797143 @default.
• W2938492869 cites W2032846834 @default.
• W2938492869 cites W2034443188 @default.
• W2938492869 cites W2038088045 @default.
• W2938492869 cites W2041208164 @default.
• W2938492869 cites W2041902939 @default.
• W2938492869 cites W2061877716 @default.
• W2938492869 cites W2075893334 @default.
• W2938492869 cites W2078741666 @default.
• W2938492869 cites W2084980103 @default.
• W2938492869 cites W2087315722 @default.
• W2938492869 cites W2090029279 @default.
• W2938492869 cites W2105276017 @default.
• W2938492869 cites W2106008153 @default.
• W2938492869 cites W2113512933 @default.
• W2938492869 cites W2138408594 @default.
• W2938492869 cites W2140602065 @default.
• W2938492869 cites W2150897391 @default.
• W2938492869 cites W2152928439 @default.
• W2938492869 cites W2154379021 @default.
• W2938492869 cites W2167069495 @default.
• W2938492869 cites W2167623001 @default.
• W2938492869 cites W2172472270 @default.
• W2938492869 cites W2175723489 @default.
• W2938492869 cites W2177724817 @default.
• W2938492869 cites W2229386619 @default.
• W2938492869 cites W2257295022 @default.
• W2938492869 cites W2261376551 @default.
• W2938492869 cites W2432771786 @default.
• W2938492869 cites W2460696518 @default.
• W2938492869 cites W2515861268 @default.
• W2938492869 cites W2567325936 @default.
• W2938492869 cites W2617875100 @default.
• W2938492869 cites W2746978450 @default.
• W2938492869 cites W2750486877 @default.
• W2938492869 cites W2791272968 @default.
• W2938492869 cites W2793316477 @default.
• W2938492869 doi "https://doi.org/10.1002/joc.6100" @default.
• W2938492869 hasPublicationYear "2019" @default.
• W2938492869 type Work @default.
• W2938492869 sameAs 2938492869 @default.
• W2938492869 citedByCount "3" @default.
• W2938492869 countsByYear W29384928692020 @default.
• W2938492869 countsByYear W29384928692021 @default.
• W2938492869 countsByYear W29384928692022 @default.
• W2938492869 crossrefType "journal-article" @default.
• W2938492869 hasAuthorship W2938492869A5000139565 @default.
• W2938492869 hasAuthorship W2938492869A5007247287 @default.
• W2938492869 hasAuthorship W2938492869A5031805159 @default.
• W2938492869 hasAuthorship W2938492869A5047358306 @default.
• W2938492869 hasAuthorship W2938492869A5047669781 @default.
• W2938492869 hasConcept C107054158 @default.
• W2938492869 hasConcept C109007969 @default.
• W2938492869 hasConcept C114793014 @default.
• W2938492869 hasConcept C121332964 @default.
• W2938492869 hasConcept C127313418 @default.
• W2938492869 hasConcept C12997251 @default.
• W2938492869 hasConcept C153294291 @default.
• W2938492869 hasConcept C166957645 @default.
• W2938492869 hasConcept C191935318 @default.
• W2938492869 hasConcept C205649164 @default.
• W2938492869 hasConcept C26873012 @default.
• W2938492869 hasConcept C2778712887 @default.
• W2938492869 hasConcept C39432304 @default.
• W2938492869 hasConcept C49204034 @default.
• W2938492869 hasConcept C97355855 @default.
• W2938492869 hasConceptScore W2938492869C107054158 @default.
• W2938492869 hasConceptScore W2938492869C109007969 @default.
• W2938492869 hasConceptScore W2938492869C114793014 @default.
• W2938492869 hasConceptScore W2938492869C121332964 @default.
• W2938492869 hasConceptScore W2938492869C127313418 @default.
• W2938492869 hasConceptScore W2938492869C12997251 @default.
• W2938492869 hasConceptScore W2938492869C153294291 @default.
• W2938492869 hasConceptScore W2938492869C166957645 @default.
• W2938492869 hasConceptScore W2938492869C191935318 @default.
• W2938492869 hasConceptScore W2938492869C205649164 @default.

• next