Delineating the Seasonally Modulated Nonlinear Feedback Onto ENSO From Tropical Instability Waves
Abstract
Tropical instability waves (TIWs), the dominant form of eddy variability in the tropics, have a peak period at about 5 weeks and are strongly modulated by both the seasonal cycle and El Niño-Southern Oscillation (ENSO). In this study, we first demonstrated that TIW-induced nonlinear dynamical heating (NDH) is basically proportional to the TIW amplitude depicted by a complex index for TIW. We further delineated that this NDH, capturing the seasonally modulated nonlinear feedback of TIW activity onto ENSO, is well approximated by a theoretical formulation derived analytically from a simple linear stochastic model for the TIW index. The results of this study may be useful for the climate community to evaluate and understand the TIW-ENSO multiscale interaction.
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Geophysical Research Letters - 2020 - Xue - Delineating the Seasonally Modulated Nonlinear Feedback Onto ENSO From Tropical.pdf (2.32 Mo)
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