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- W200409462 abstract "Recent studies indicate that coupled general circulation models (GCM) display mixed success in simulating the properties of the El Nino/Southern Oscillation (ENSO). Specifically, aggregate runs of various GCMs typically show spatial and temporal disparities compared to observations. We turn to the Zebiak-Cane model of intermediate complexity for the tropical Pacific ocean to study the response of the sea surface temperature (SST) and inter-annual variability of ENSO under different wind stress conditions. Spatial variation is modeled after the meridional structure of the zonal wind stress based on TAO/TRITON measurements, and furthermore on reconstructed Pliocene conditions from the HadCM3 PlioMIP Exp 2 wind data. Temporal variations are introduced with a simple seasonal cycle. Among all conditions simulated, only very weak trade winds result in a ”permanent” El Nino with weak SST gradients and no variability. A cold tongue (CT) structure is always present when the wind is above a minimum critical value, although the oscillations vanish if the wind crosses a threshold maximum value. Apart from these extremes, periods of 3 ∼ 4 years are found with ∆SST amplitudes of 5◦C ∼ 9◦C ." @default.
- W200409462 created "2016-06-24" @default.
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- W200409462 date "2014-02-26" @default.
- W200409462 modified "2023-09-27" @default.
- W200409462 title "Wind stress and ENSO dynamics" @default.
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