Related Experiment Video
Updated: May 24, 2025

06:10
Using Generative Art to Convey Past and Future Climate Transitions
Published on: March 31, 2023
854
Marine ecosystem role in setting up preindustrial and future climate
Jerry F Tjiputra1, Damien Couespel2, Richard Sanders2
1NORCE Norwegian Research Centre AS, Bjerknes Centre for Climate Research, Bergen, Norway. jetj@norceresearch.no.
Nature Communications
|March 5, 2025
Summary
The ocean
Area of Science:
- Earth system science
- Oceanography
- Climate science
Background:
- The ocean is a critical component of the global carbon cycle, influencing atmospheric CO2 levels.
- Current models often simplify the complex land-ocean feedback mechanisms.
- Understanding ocean biology's role is essential for accurate climate projections.
Purpose of the Study:
- To investigate the intricate role of ocean biology in regulating atmospheric CO2.
- To assess the impact of shutting down the ocean's biological pump on global carbon levels.
- To explore the coupled land-ocean feedback in Earth system modeling.
Main Methods:
- Utilized an interactive Earth system model to simulate changes in the carbon cycle.
- Analyzed the new equilibrium state of atmospheric CO2 after disabling the ocean's biological pump.
- Quantified carbon exchange between the ocean and land components of the model.
Main Results:
- Atmospheric CO2 increased by over 50% (163 ppm) when the ocean's biological pump was shut down.
- Approximately half of the carbon released from the ocean was adsorbed by land.
- The abiotic ocean showed reduced capacity for anthropogenic carbon uptake due to warming and altered surface conditions.
Conclusions:
- Ocean biology plays a more complex role in carbon sequestration than previously understood.
- Land-ocean feedbacks significantly influence atmospheric CO2 responses to changes in marine ecosystems.
- Preserving marine ecosystem functioning is vital for climate change mitigation efforts.
Related Concept Videos
Global Climate Change
24.1K
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.
24.1K
What is Climate?
18.2K
Climate refers to the prevailing weather conditions in a specific area over an extended period. As the saying goes, “Climate is what you expect. Weather is what you get.” Climate is influenced by geographic factors, such as latitude, terrain, and proximity to bodies of water.
18.2K
What is an Ecosystem?
39.2K
Overview
39.2K
Primary Production
23.5K
The total amount of energy acquired by primary producers in an ecosystem is called gross primary production (GPP). However, of this energy, producers use some for metabolic processes, and some is lost as heat, decreasing the amount of energy available to the next trophic level. The remaining usable amount of energy is called the net primary productivity (NPP). In terrestrial ecosystems, NPP is driven by climate, while light penetration and nutrient availability drive NPP in aquatic ecosystems.
23.5K
The Carbon Cycle
36.9K
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.
36.9K
What are Biogeochemical Cycles?
30.9K
The most common elements in organic molecules, carbon, hydrogen, oxygen, nitrogen, sulfur, and phosphorus, are only available in the ecosystem in limited amounts. Therefore, these nutrients must be recycled through both biotic and abiotic components of the ecosystem, in processes generally called biogeochemical cycles.
30.9K

