Hi everyone,
I am currently working on modifying iron inputs in CESM2’s ocean biogeochemistry (POP2 + MARBL), and I would like to understand exactly how iron_flux is converted into tracer tendencies for dissolved iron (Fe) inside the model(e.g., mmol Fe m⁻³ s⁻¹).
I am currently working on modifying iron inputs in CESM2’s ocean biogeochemistry (POP2 + MARBL), and I would like to understand exactly how iron_flux is converted into tracer tendencies for dissolved iron (Fe) inside the model(e.g., mmol Fe m⁻³ s⁻¹).