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Zonal phase propagation of ENSO sea surface temperature anomalies: Revisited

机译:ENSO海面温度异常的带状相传播:再探讨

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摘要

Previous studies have identified a reversal in the phase propagation characteristics (from westward to eastward propagation) of the El Ni?o-Southern Oscillation (ENSO) during the 1976 climate shift. These studies relied on the assumption of a stationary seasonal cycle in Sea Surface Temperature (SST), ignoring the possible effect of ENSO and decadal variability on the seasonal cycle strength. Here we demonstrate using complex empirical orthogonal functions combined with Radon transform methods that mutidecadal amplitude modulations of the seasonal cycle, the semiannual cycle, and the El Ni?o Modoki mode played an important role in determining the phase propagation characteristics of equatorial SST anomalies in past decades. We find very little evidence for changes in the propagation characteristics of the Cold Tongue ENSO mode.
机译:先前的研究已经确定了1976年气候变化期间厄尔尼诺-南方涛动(ENSO)的相位传播特征(从西向东传播)发生了逆转。这些研究是基于海面温度(SST)稳定的季节性周期的假设,而忽略了ENSO和年代际变化对季节性周期强度的可能影响。在这里,我们展示了使用复杂的经验正交函数与Radon变换方法相结合的方法,该方法过去对季节性周期,半年周期和El Ni?o Modoki模式的半年代振幅调制在确定赤道SST异常的相位传播特征中起着重要作用。几十年。我们很少发现冷舌ENSO模式传播特性发生变化的证据。

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