It is extremely important to estimate the
primary production of phytoplankton when considering the carbon cycle in
the ocean. The increase of seawater temperature associated with global
warming in recent years is thought to affect the primary productivity of
the ocean. However, the conventional primary productivity estimation
method uses sea surface temperature as an input variable, and it is
difficult to correctly discuss the change in primary production due to
global warming. Therefore, we designed a method of estimating primary production
using the light absorption coefficient of phytoplankton, which is a
parameter independent of seawater temperatures.

Figure. (a) Basic production estimated by the method
based on the light absorption coefficient, (b) basic production estimated by the
conventional method, and (c) difference between a and b.