SUMMARY
The amount of phytoplankton in seawater, particularly around reefs and near the surface, is typically measured using satellite telemetry based on chlorophyll levels, which are then converted to biomass. Phytoplankton biomass is highly variable, with significant fluctuations occurring during algal blooms in late spring and late summer. Estimates indicate that phytoplankton contributes approximately 1% of the global biomass, translating to about 5 billion metric tons of carbon in the oceans. Measurements are influenced by factors such as vertical distribution and time of day, with the highest concentrations found within 30 meters of the surface during midday.
PREREQUISITES
- Understanding of chlorophyll measurement techniques
- Familiarity with satellite telemetry for biomass estimation
- Knowledge of algal bloom dynamics in marine ecosystems
- Basic concepts of vertical distribution in aquatic environments
NEXT STEPS
- Research satellite telemetry methods for measuring chlorophyll levels
- Explore the dynamics of algal blooms in temperate waters
- Investigate the impact of vertical distribution on phytoplankton biomass measurements
- Learn about bathymetric devices used for sampling water and depth
USEFUL FOR
Marine biologists, ecologists, environmental scientists, and anyone interested in understanding phytoplankton dynamics and their role in marine ecosystems.