Extended Data Fig. 6: Each term in Eq. (4) plotted as a contribution to ΔLAI anomaly in the response to 2015-2016 El Niño.
From: Global mangrove growth variability driven by climatic oscillation-induced sea-level fluctuations
The contribution is calculated as the product of mangrove sensitivity to (a) air temperature, (b) SPEI, (c) wind speed, (d) sea surface temperature, (e) sea surface salinity, and (f) sea-level anomaly and El Niño-induced anomaly in these factors.
