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- W2555691906 abstract "Ocean dynamics have been demonstrated to play a dominant role in the variability of tropical climate system on seasonal to interannual time scales. By coupling with the atmosphere, they give rise to the well-known El Nino-Southern Oscillation phenomenon. However, on longer-than-interannual time scales, the role of ocean dynamics is still in debate. Clement et al. (2011) argued that interactive ocean dynamics are not required to produce the Southern Oscillation (SO). They analyzed simulations with atmospheric general circulation models that have varying degrees of coupling to the ocean and proved that the SO emerges as a dominant mode of variability (defined in their paper as the thermally coupled Walker (TCW) mode) if the atmosphere and ocean are coupled only through heat and moisture fluxes (not coupled dynamically). They also showed that the spatial patterns of sea surface temperature (SST) and sea level pressure (SLP) variability associated with the TCW (Fig. 1) are remarkably realistic. In the absence of interactive ocean dynamics, Clement et al. hypothesized that an off-equatorial trade wind-evaporation-SST (WES) feedback and cloud shortwave radiative effects in the central Pacific are responsible for the anomalous pattern shown in Fig. 1. To test their hypothesis, we have investigated the physical mechanisms of El Nino-like warming events as shown in Fig. 1 by analyzing simulations with atmospheric general circulation models coupled to a 50m slab mixed layer ocean (AGCM-slab). Figure 1. The multimodel-mean composite of SST, SLP and surface wind anomalies at the time when the Nino3.4 SST anomaly peaks during an El Nino-like warming event." @default.
- W2555691906 created "2016-11-30" @default.
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- W2555691906 date "2011-01-01" @default.
- W2555691906 modified "2023-09-23" @default.
- W2555691906 title "The physical mechanisms of El Nino-like warming events in the coupled slab ocean-atmospheric general circulation models" @default.
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- W2555691906 hasPublicationYear "2011" @default.
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