Phytoplankton biomass in seawater, particularly around reefs and near the surface, is typically measured using satellite telemetry that assesses chlorophyll levels, which are then converted to biomass estimates. This biomass is highly variable, influenced by seasonal algal blooms in temperate waters, with significant fluctuations occurring throughout the year. Phytoplankton is generally concentrated within the upper 30 meters of the water column, with the highest concentrations found near the surface during midday. Global estimates suggest that the total biomass of phytoplankton in the oceans is around 5 to 10 billion tonnes of carbon, representing about 1% of the global biomass. In smaller, closed systems like ponds, phytoplankton concentrations are often reported in terms of chlorophyll content, which can then be used to derive biomass estimates. Overall, the measurement of phytoplankton is complex and subject to significant temporal and spatial variability.