Correction : Geoscience Letters (2023) 10:23  https://doi.org/10.1186/s40562-023-00277-8

Following publication of the original article (Lagare et al. 2023), the authors would like to correct the errors in Figs. 5 and 9 labels and some references.

The authors have identified that Figs. 5 and 9 were mislabeled.

Fig. 5
figure 5

Spatial distributions of 9 h of accumulated a observation and b–f model rainfall (14:00–23:00 LST of 03 May 2017) at different horizontal resolutions, and g area-averaged hourly mean rainfall over the area in a; h threat scores at different threshold values of the 9 h of accumulated rainfall in a–f

Full size image
Fig. 9
figure 9

Schematic diagram demonstrating the development of MCSs. Sea breeze on the western coast supplied the abundant moisture that developed MCS-1 in the basin. The precipitating downdrafts of MCS-1 formed cold pools that contributed to its upscale growth. The interaction of the southeasterly winds and Mount Apo terrain developed MCS-2, and its precipitating downdrafts formed a cold pool that assisted its maintenance and growth

Full size image

It has been corrected in this correction.

The original article has been updated.


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