Matches in SemOpenAlex for { <https://semopenalex.org/work/W2085286775> ?p ?o ?g. }
- W2085286775 endingPage "1596" @default.
- W2085286775 startingPage "1573" @default.
- W2085286775 abstract "The evolution of the dipole mode (DM) events in the Indian Ocean is examined using an ocean model that is driven by the NCEP fluxes for the period 1975–1998. The positive DM events during 1997, 1994 and 1982 and negative DM events during 1996 and 1984–1985 are captured by the model and it reproduces both the surface and subsurface features associated with these events. In its positive phase, the DM is characterized by warmer than normal SST in the western Indian Ocean and cooler than normal SST in the eastern Indian Ocean. The DM events are accompanied by easterly wind anomalies along the equatorial Indian Ocean and upwelling-favorable alongshore wind anomalies along the coast of Sumatra. The Wyrtki jets are weak during positive DM events, and the thermocline is shallower than normal in the eastern Indian Ocean and deeper in the west. This anomaly pattern reverses during negative DM events. During the positive phase of the DM easterly wind anomalies excite an upwelling equatorial Kelvin wave. This Kelvin wave reflects from the eastern boundary as an upwelling Rossby wave which propagates westward across the equatorial Indian Ocean. The anomalies in the eastern Indian Ocean weaken after the Rossby wave passes. A similar process excites a downwelling Rossby wave during the negative phase. This Rossby wave is much weaker but wind forcing in the central equatorial Indian Ocean amplifies the downwelling and increases its westward phase speed. This Rossby wave initiates the deepening of the thermocline in the western Indian Ocean during the following positive phase of the DM. Rossby wave generated in the southern tropical Indian Ocean by Ekman pumping contributes to this warming. Concurrently, the temperature equation of the model shows upwelling and downwelling to be the most important mechanism during both positive events of 1994 and 1997." @default.
- W2085286775 created "2016-06-24" @default.
- W2085286775 creator A5003579165 @default.
- W2085286775 creator A5028627532 @default.
- W2085286775 creator A5050266619 @default.
- W2085286775 date "2002-01-01" @default.
- W2085286775 modified "2023-10-12" @default.
- W2085286775 title "Indian Ocean dipole mode events in an ocean general circulation model" @default.
- W2085286775 cites W1966780503 @default.
- W2085286775 cites W1973776704 @default.
- W2085286775 cites W1975601006 @default.
- W2085286775 cites W1981669700 @default.
- W2085286775 cites W1985669309 @default.
- W2085286775 cites W1985834492 @default.
- W2085286775 cites W2003526577 @default.
- W2085286775 cites W2004609797 @default.
- W2085286775 cites W2008017701 @default.
- W2085286775 cites W2013805629 @default.
- W2085286775 cites W2017759254 @default.
- W2085286775 cites W2018881311 @default.
- W2085286775 cites W2026745039 @default.
- W2085286775 cites W2031127053 @default.
- W2085286775 cites W2039177040 @default.
- W2085286775 cites W2060935889 @default.
- W2085286775 cites W2061882206 @default.
- W2085286775 cites W2064125711 @default.
- W2085286775 cites W2064376429 @default.
- W2085286775 cites W2070794850 @default.
- W2085286775 cites W2082001988 @default.
- W2085286775 cites W2082648492 @default.
- W2085286775 cites W2091390698 @default.
- W2085286775 cites W2091875832 @default.
- W2085286775 cites W2093701912 @default.
- W2085286775 cites W2111418993 @default.
- W2085286775 cites W2126851605 @default.
- W2085286775 cites W2173251738 @default.
- W2085286775 cites W2173725642 @default.
- W2085286775 cites W2179982747 @default.
- W2085286775 doi "https://doi.org/10.1016/s0967-0645(01)00157-6" @default.
- W2085286775 hasPublicationYear "2002" @default.
- W2085286775 type Work @default.
- W2085286775 sameAs 2085286775 @default.
- W2085286775 citedByCount "157" @default.
- W2085286775 countsByYear W20852867752012 @default.
- W2085286775 countsByYear W20852867752013 @default.
- W2085286775 countsByYear W20852867752014 @default.
- W2085286775 countsByYear W20852867752015 @default.
- W2085286775 countsByYear W20852867752016 @default.
- W2085286775 countsByYear W20852867752017 @default.
- W2085286775 countsByYear W20852867752018 @default.
- W2085286775 countsByYear W20852867752019 @default.
- W2085286775 countsByYear W20852867752020 @default.
- W2085286775 countsByYear W20852867752021 @default.
- W2085286775 countsByYear W20852867752022 @default.
- W2085286775 countsByYear W20852867752023 @default.
- W2085286775 crossrefType "journal-article" @default.
- W2085286775 hasAuthorship W2085286775A5003579165 @default.
- W2085286775 hasAuthorship W2085286775A5028627532 @default.
- W2085286775 hasAuthorship W2085286775A5050266619 @default.
- W2085286775 hasConcept C105824904 @default.
- W2085286775 hasConcept C111368507 @default.
- W2085286775 hasConcept C119601563 @default.
- W2085286775 hasConcept C122523270 @default.
- W2085286775 hasConcept C127313418 @default.
- W2085286775 hasConcept C12980444 @default.
- W2085286775 hasConcept C132651083 @default.
- W2085286775 hasConcept C13280743 @default.
- W2085286775 hasConcept C134097258 @default.
- W2085286775 hasConcept C141452985 @default.
- W2085286775 hasConcept C142672198 @default.
- W2085286775 hasConcept C145151356 @default.
- W2085286775 hasConcept C149348798 @default.
- W2085286775 hasConcept C150320492 @default.
- W2085286775 hasConcept C176341353 @default.
- W2085286775 hasConcept C187599188 @default.
- W2085286775 hasConcept C187850051 @default.
- W2085286775 hasConcept C197968181 @default.
- W2085286775 hasConcept C2781281996 @default.
- W2085286775 hasConcept C49204034 @default.
- W2085286775 hasConcept C62897925 @default.
- W2085286775 hasConcept C73421765 @default.
- W2085286775 hasConceptScore W2085286775C105824904 @default.
- W2085286775 hasConceptScore W2085286775C111368507 @default.
- W2085286775 hasConceptScore W2085286775C119601563 @default.
- W2085286775 hasConceptScore W2085286775C122523270 @default.
- W2085286775 hasConceptScore W2085286775C127313418 @default.
- W2085286775 hasConceptScore W2085286775C12980444 @default.
- W2085286775 hasConceptScore W2085286775C132651083 @default.
- W2085286775 hasConceptScore W2085286775C13280743 @default.
- W2085286775 hasConceptScore W2085286775C134097258 @default.
- W2085286775 hasConceptScore W2085286775C141452985 @default.
- W2085286775 hasConceptScore W2085286775C142672198 @default.
- W2085286775 hasConceptScore W2085286775C145151356 @default.
- W2085286775 hasConceptScore W2085286775C149348798 @default.
- W2085286775 hasConceptScore W2085286775C150320492 @default.
- W2085286775 hasConceptScore W2085286775C176341353 @default.
- W2085286775 hasConceptScore W2085286775C187599188 @default.
- W2085286775 hasConceptScore W2085286775C187850051 @default.