FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2134026697> ?p ?o ?g. }

• W2134026697 endingPage "3165" @default.
• W2134026697 startingPage "3165" @default.
• W2134026697 abstract "Dominant phase relationships between sea surface temperature (SST), high cloud cover (HCC), and zonal wind at 850 mbar on intraseasonal and interannual time scales in the warm pool region of the western Pacific are examined. Using the complex empirical orthogonal function (CEOF) analysis, two air-sea coupled modes, that is, an intraseasonal mode and an interannual mode, are statistically extracted. It is found that in the intraseasonal mode the area of maximum SST anomaly lies to the east of the center of the active large-scale convection area and therefore positive SST anomalies exist at the easterly anomaly area. The existence of high SST at the easterly anomaly area provides a favorable condition for a large-scale disturbance to propagate eastward, though the evaporation-wind feedback mechanism may also favor its eastward propagation if the mean wind is easterly. It is seen that the intraseasonal mode is very similar to the advective mode proposed by Lau and Shen (1988) with respect to the phase relationship. However, since the time evolution of the intraseasonal mode does not always coincide with the variations of east-west SST gradient over the tropical western Pacific, this mode requires another mechanism other than the east-west SST advection causing the advective mode. On one hand, the interannual mode has a characteristic that the phase relation of 850 mbar zonal wind (u) is different in each region of the tropical western Pacific, whereas the SST is almost in phase with HCC. The predominant growth of the mode defined in the key region (0°–10°N, 130°–160°E) corresponds to the life cycle that occurs when the El Niño/Southern Oscillation (ENSO) begins, develops, and decays. This verifies that the ENSO is one of the prominent phenomena in the air-sea interactive system on the interannual time scale. On the other hand, the mode over the tropical Pacific around the dateline explains the air-sea coupling when large-scale convection is not very active. It is thus clear that evident differences of air-sea coupling exist between the intraseasonal time scale and the interannual time scale. It is also determined that the strength of air-sea coupling varies with year in both time scales. The above results provide a clue for understanding the mechanism of multiscale air-sea coupling in the tropics." @default.
• W2134026697 created "2016-06-24" @default.
• W2134026697 creator A5005660243 @default.
• W2134026697 date "1991-01-01" @default.
• W2134026697 modified "2023-09-24" @default.
• W2134026697 title "Air-sea coupled modes on intraseasonal and interannual time scales over the tropical western Pacific" @default.
• W2134026697 cites W167081520 @default.
• W2134026697 cites W191763913 @default.
• W2134026697 cites W194847632 @default.
• W2134026697 cites W1967709875 @default.
• W2134026697 cites W197828200 @default.
• W2134026697 cites W1980681647 @default.
• W2134026697 cites W1992132562 @default.
• W2134026697 cites W2006552603 @default.
• W2134026697 cites W2010957707 @default.
• W2134026697 cites W2050045353 @default.
• W2134026697 cites W2053025896 @default.
• W2134026697 cites W2058221234 @default.
• W2134026697 cites W2072941362 @default.
• W2134026697 cites W2074428993 @default.
• W2134026697 cites W2077615224 @default.
• W2134026697 cites W2085091203 @default.
• W2134026697 cites W2087523203 @default.
• W2134026697 cites W2089640918 @default.
• W2134026697 cites W2290934095 @default.
• W2134026697 cites W41667157 @default.
• W2134026697 cites W85681110 @default.
• W2134026697 doi "https://doi.org/10.1029/90jc01845" @default.
• W2134026697 hasPublicationYear "1991" @default.
• W2134026697 type Work @default.
• W2134026697 sameAs 2134026697 @default.
• W2134026697 citedByCount "7" @default.
• W2134026697 crossrefType "journal-article" @default.
• W2134026697 hasAuthorship W2134026697A5005660243 @default.
• W2134026697 hasConcept C10899652 @default.
• W2134026697 hasConcept C111919701 @default.
• W2134026697 hasConcept C121332964 @default.
• W2134026697 hasConcept C127313418 @default.
• W2134026697 hasConcept C12997251 @default.
• W2134026697 hasConcept C134097258 @default.
• W2134026697 hasConcept C13724139 @default.
• W2134026697 hasConcept C153294291 @default.
• W2134026697 hasConcept C26873012 @default.
• W2134026697 hasConcept C39432304 @default.
• W2134026697 hasConcept C41008148 @default.
• W2134026697 hasConcept C48677424 @default.
• W2134026697 hasConcept C49204034 @default.
• W2134026697 hasConcept C5072599 @default.
• W2134026697 hasConcept C91586092 @default.
• W2134026697 hasConcept C97355855 @default.
• W2134026697 hasConceptScore W2134026697C10899652 @default.
• W2134026697 hasConceptScore W2134026697C111919701 @default.
• W2134026697 hasConceptScore W2134026697C121332964 @default.
• W2134026697 hasConceptScore W2134026697C127313418 @default.
• W2134026697 hasConceptScore W2134026697C12997251 @default.
• W2134026697 hasConceptScore W2134026697C134097258 @default.
• W2134026697 hasConceptScore W2134026697C13724139 @default.
• W2134026697 hasConceptScore W2134026697C153294291 @default.
• W2134026697 hasConceptScore W2134026697C26873012 @default.
• W2134026697 hasConceptScore W2134026697C39432304 @default.
• W2134026697 hasConceptScore W2134026697C41008148 @default.
• W2134026697 hasConceptScore W2134026697C48677424 @default.
• W2134026697 hasConceptScore W2134026697C49204034 @default.
• W2134026697 hasConceptScore W2134026697C5072599 @default.
• W2134026697 hasConceptScore W2134026697C91586092 @default.
• W2134026697 hasConceptScore W2134026697C97355855 @default.
• W2134026697 hasIssue "S01" @default.
• W2134026697 hasLocation W21340266971 @default.
• W2134026697 hasOpenAccess W2134026697 @default.
• W2134026697 hasPrimaryLocation W21340266971 @default.
• W2134026697 hasRelatedWork W1972175540 @default.
• W2134026697 hasRelatedWork W2366892875 @default.
• W2134026697 hasRelatedWork W2386245437 @default.
• W2134026697 hasRelatedWork W2386322423 @default.
• W2134026697 hasRelatedWork W2941318649 @default.
• W2134026697 hasRelatedWork W3036313000 @default.
• W2134026697 hasRelatedWork W3081257409 @default.
• W2134026697 hasRelatedWork W3130622650 @default.
• W2134026697 hasRelatedWork W4385773964 @default.
• W2134026697 hasRelatedWork W45555295 @default.
• W2134026697 hasVolume "96" @default.
• W2134026697 isParatext "false" @default.
• W2134026697 isRetracted "false" @default.
• W2134026697 magId "2134026697" @default.
• W2134026697 workType "article" @default.