The compensation depth between photosynthesis and respiration of phytoplankton in the ocean must be dependent on some factors: the illumination at the surface, the transparency of the water, the biological character of the plankton present, and the temperature. The compensation point was found nearer to the surface as you move closer to the coast. It is also lower in the winter seasons in the Baltic Sea according to a study that examined the compensation point of multiple photosynthetic species. The blue portion of the visible spectrum, between 455 and 495 nanometers, dominates light at the compensation depth.