The publisher regrets that, due to a proofreading error, edits made to paragraph 1, page 7, were not included in the version of record online. The correct paragraph can be seen below:
Figure 3(b) estimates the continuity of the wet season according to each rainfall dataset by plotting the longest continuous run of days per hydrological year (01 September–31 August) where rainfall exceeds a threshold of either 1, 5, or 10 mm on each day. This shows some similarity with Figure 3(a). For example, Yanto has many more runs of days with >1 or >5 mm rainfall than any other dataset, but this matches its middling annual rainfall total because it also has the smallest top 100 events. This result implies that wet-season rainfall in Yanto is distributed more evenly across days, while in other datasets, particularly MSWEP, wet-season rainfall is more concentrated in fewer days. In general, there is an inverse relationship between a dataset's top 100 daily totals and its longest run of days with >1 or >5 mm rainfall. This relationship is subdued when a dry/wet threshold of 10 mm is considered because 10 mm/day is approximately the mean daily rainfall for the wet season, and many daily rainfalls must be below the mean by definition. However, the pattern seen using a 10 mm threshold is still similar to those observed using a 1 or 5 mm threshold.
