Fig. 4: Seasonal heterogeneity of phytoplankton response to strong submesoscale ageostrophic motion.
From: Heterogeneity of phytoplankton response to submesoscale processes in the global ocean
a-c Geographic distributions of (a) \({r}_{{Chl}}\), (b) \({r}_{{C}_{{Phyto}}}\) and (c) \({r}_{\theta }\) when strong submesoscale ageostrophic motions happen with positive \({r}_{{Chl}}\) in summer (June to September in the Northern Hemisphere, December to March in the Southern Hemisphere). d–f Same as (a–c) but for winter (December to March in the Northern Hemisphere, June to September in the Southern Hemisphere).
