Related Experiment Video
Updated: Jul 18, 2026

10:43
Unraveling the Unseen Players in the Ocean - A Field Guide to Water Chemistry and Marine Microbiology
Published on: November 5, 2014
Anthropogenic CO2 uptake by the ocean based on the global chlorofluorocarbon data set
Ben I McNeil1, Richard J Matear, Robert M Key
1Atmospheric and Oceanic Science Program, Princeton University, Princeton, NJ 08544, USA.
Summary
The ocean absorbed significant amounts of anthropogenic carbon dioxide (CO2), storing 14.8 and 17.9 petagrams between 1980-1989 and 1990-1999, respectively. This indicates a higher CO2 uptake than many ocean models predict.
Area of Science:
- Oceanography
- Climate Science
- Biogeochemistry
Background:
- Anthropogenic carbon dioxide (CO2) emissions significantly impact global carbon cycles.
- Accurate estimation of oceanic CO2 uptake is crucial for understanding climate change.
- Previous methods for quantifying oceanic CO2 inventory have limitations.
Purpose of the Study:
- To estimate the oceanic inventory of anthropogenic CO2 from 1980 to 1999.
- To determine the decadal oceanic net uptake of anthropogenic carbon.
- To compare estimated oceanic CO2 uptake with predictions from ocean general circulation models.
Main Methods:
- Utilized a technique based on the global chlorofluorocarbon (CFC) dataset.
- Analyzed carbon storage in the ocean over two distinct decadal periods.
- Calculated the annual net uptake of carbon dioxide by the ocean.
Main Results:
- The ocean stored 14.8 petagrams of anthropogenic carbon from mid-1980 to mid-1989.
- The ocean stored 17.9 petagrams of anthropogenic carbon from mid-1990 to mid-1999.
- Oceanwide net uptake rates were estimated at 1.6 and 2.0 +/- 0.4 petagrams of carbon per year for the respective decades.
Conclusions:
- The study provides an upper limit for the solubility-driven anthropogenic CO2 flux into the ocean.
- Results suggest that many ocean general circulation models overestimate oceanic anthropogenic CO2 uptake.
- This research refines our understanding of the ocean's role in mitigating atmospheric CO2 levels.
More Related Videos
Related Concept Videos
The Carbon Cycle
Carbon is the basis of all organic matter on Earth, and is recycled through the ecosystem in two primary processes: one in which carbon is exchanged among living organisms, and one in which carbon is cycled over long periods of time through fossilized organic remains, weathering of rocks, and volcanic activity. Human activities, including increased agricultural practices and the burning of fossil fuels, has greatly affected the balance of the natural carbon cycle.
Global Climate Change
Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
Sustainable Development
As the human population continues to grow and use resources, we must be mindful of our planet’s natural limits. Sustainable development provides a pathway to maintain and improve human life now while also ensuring that future generations will have the resources that they need. The long-term success of sustainability efforts rests on understanding the interplay between human actions and ecological systems.
Radiation: Applications
The average temperature of Earth is the subject of much current discussion. Earth is in radiative contact with both the Sun and dark space; it receives almost all its energy from the radiation of the Sun and reflects some of it into outer space. Dark space is very cold, about 3 K, so Earth radiates energy into it. For instance, heat transfer occurs from soil and grasses, the rate of which can be so rapid that frost can occur on clear summer evenings, even in warm latitudes.
The average...
The average...
Marine Microbial Ecology
Marine microbial ecosystems are shaped by distinct physicochemical limits, including high salinity, low nutrient availability, and fluctuating oxygen levels. These conditions favor smaller microbial cell sizes, which maximize their surface-to-volume ratio for efficient nutrient uptake.Microbial activity and community composition are closely linked to biogeochemical cycles, particularly in dynamic environments like estuaries, where halotolerant microbes thrive in response to variable salinity...
Microbes and Climate Change
Microorganisms are pivotal agents in Earth's biogeochemical cycles, significantly influencing climate dynamics through their metabolic activities. These microbes modulate the levels of key greenhouse gases by both contributing to and helping mitigate climate change.Microbial Contributions to Greenhouse Gas EmissionsRising global temperatures accelerate microbial metabolism, which, in turn, speeds up the decomposition of organic matter. This process releases carbon dioxide (CO₂) through...

