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Correction to: Impact of the observed SST frequency in the model initialization on the BSISO prediction

The Original Article was published on 19 April 2021

Correction to: Climate Dynamics https://doi.org/10.1007/s00382-021-05761-5

In the original version of the article, the mathematical formula in Sect. 2.4 and the Fig. 14 has been wrongly published. The correct formula and Fig. 14 is given below:


(1) Mathematic Formula (to replace the second formula in Sect. 2.4 of paper)

$$ \frac{{\partial \langle{m}\rangle}}{{\partial t}} = - ~\left\langle {V \cdot \nabla m} \right\rangle - \left\langle {\omega \cdot \frac{{\partial m}}{{\partial p}}} \right\rangle + \left\langle {LW} \right\rangle + \left\langle {SW} \right\rangle + LH + SH $$

(2) Figure 14 (to replace the old Fig. 14 of paper).

Fig. 14
figure14

Same as in Fig. 11, but for the intraseasonal anomalies of a precipitation and b surface latent heat fux for the strong BSISO cases with wet-to-dry (WD), persistent-wet (PW) and persistent-dry (PD) phase variation

The original article has been updated.

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Correspondence to Xiangwen Liu or Anning Huang.

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Zhu, X., Liu, X., Huang, A. et al. Correction to: Impact of the observed SST frequency in the model initialization on the BSISO prediction. Clim Dyn 57, 1119–1120 (2021). https://doi.org/10.1007/s00382-021-05844-3

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