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

1 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

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.