Figure 4
From: Madden–Julian Oscillation Enhances Phytoplankton Biomass in the Maritime Continent
(a) Domain-averaged anomalous value of Chl (blue line), TSM(red line), and Chl increase rate (dash line) over the Banda Sea (between 126°–136°E) in the eight MJO phases; (b) scatter plots of Chl versus integrated surface-water convergence (left) and TSM (right), based on the daily anomalous value during winter in 2002–2010 (total of 720 days). All correlation coefficients are significant at the 0.05 level.
