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It is not fixed in the atmosphere. It moves as part of the carbon cycle in and out of the oceans, the atmosphere and the land.
False.
The formation of seas and oceans helped to regulate the amount of carbon dioxide in the atmosphere by absorbing and storing it in the water. This process helped to reduce the levels of carbon dioxide in the atmosphere, which contributed to creating a more stable climate on Earth.
The oceans help provide an exchange of gases with the atmosphere by dissolving oxygen and carbon dioxide. Oxygen is essential for marine life to breathe, while carbon dioxide is important for regulating the Earth's climate through its presence in the carbon cycle.
Some carbon dioxide is absorbed by the top levels of the oceans where it is beginning to turn the oceans more acidic. That and photosynthesis are the only ways that carbon dioxide is taken out of the atmosphere. Industries that emit carbon dioxide pollution are trialling ways of trapping carbon dioxide as it goes up the chimney stacks (scrubbers).
An example of carbon moving from the atmosphere to the hydrosphere is when carbon dioxide (CO2) in the atmosphere dissolves into the oceans. This process, known as carbon sequestration, helps regulate the amount of CO2 in the atmosphere and directly impacts the ocean's acidity levels.
It is not fixed in the atmosphere. It moves as part of the carbon cycle in and out of the oceans, the atmosphere and the land.
The oceans contain about 50 times more carbon dioxide (CO2) than the atmosphere and 19 times more than the land biosphere.
Carbon sinks are natural or artificial reservoirs that absorb and store carbon dioxide from the atmosphere, such as forests and oceans. Carbon sources, on the other hand, release carbon dioxide into the atmosphere, like burning fossil fuels. The balance between carbon sinks and sources is crucial in regulating the amount of carbon dioxide in the atmosphere, which directly impacts climate change. If carbon sources exceed carbon sinks, more carbon dioxide is released into the atmosphere, leading to global warming and climate change.
The combustion of fossil fuels releases carbon dioxide into the atmosphere, contributing to the greenhouse effect and global warming. This disrupts the balance of the carbon cycle by adding more carbon dioxide than natural systems can absorb, leading to increased levels of carbon in the atmosphere and oceans.
After carbon dioxide is released into the atmosphere, it can be absorbed by plants through photosynthesis, dissolved in the oceans, or remain in the atmosphere contributing to the greenhouse effect.
When the atmosphere has excess carbon dioxide, the oceans absorb it in a process known as carbon sequestration. This is an example of a natural feedback mechanism, where the Earth's systems work to achieve a new equilibrium. However, this absorption can lead to ocean acidification, which negatively impacts marine life and ecosystems.
False.
Carbon dioxide is kept at a constant level by an exchange between the atmosphere and various sinks, such as oceans, plants, and soil. These sinks absorb and store carbon dioxide, helping to regulate levels in the atmosphere. The balance between carbon dioxide sources, such as human activities and natural processes, and sinks maintains equilibrium in the carbon cycle.
The formation of seas and oceans helped to regulate the amount of carbon dioxide in the atmosphere by absorbing and storing it in the water. This process helped to reduce the levels of carbon dioxide in the atmosphere, which contributed to creating a more stable climate on Earth.
The ocean water absorbed much of the carbon dioxide from the atmosphere.
Plants and trees absorb carbon dioxide during the process of photosynthesis. Additionally, oceans act as carbon sinks by absorbing and storing carbon dioxide from the atmosphere. Human activities such as afforestation, reforestation, and carbon capture and storage technologies also help in removing carbon dioxide from the atmosphere.