Extended Data Fig. 8: Dominant driver of sea level anomaly during climatic events.
From: Global mangrove growth variability driven by climatic oscillation-induced sea-level fluctuations
The dominant component driving SLA during (a) 2015-2016 El Niño, (b) 2010-2012 La Niña, and (c) 2019 pIOD. In (a) and (b), the left pie charts represent results from Indo-Malesia and Australasia, while in (c), the left pie chart shows results from eastern Africa. The right pie charts in (a) and (b) depict results from western America, while in (c), the right pie chart shows results from Indo-Malesia and Australasia. The red areas in the charts denote regions where SLA is predominantly influenced by climatic oscillations, and the blue areas indicate regions where the nodal cycle is the dominant factor. Specific spatial details of SLA contributed by climatic oscillations and nodal cycle are shown in Supplementary Fig. 8.
