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It is Industry that impacts global carbon dioxide emissions. Well, here we have a new Movie Title: - "BACKFIRE". There is already 'enough' Heat contained within Our Oceans ...

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What is an example for when the atmosphere carbon to the hydrosphere?

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.


How is carbon dioxide fixed in the atmosphere?

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.


How many times more carbon is in the oceans than in the atmosphere?

The oceans contain about 50 times more carbon dioxide (CO2) than the atmosphere and 19 times more than the land biosphere.


What is the relationship between carbon sinks and carbon sources in the context of climate change?

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.


What role does the combustion of fossil fuels have in the carbon cycle?

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.


Where does carbon dioxide go after it is released into the atmosphere?

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 too much carbon dioxide in it the oceans absorb some if it to achieve a new balance which is an example of what?

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.


Is The atmosphere stores much more carbon dioxide than the oceans?

False.


Carbon dioxide is kept at a constant level by an exchange between the atmosphere and?

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.


How did the formation of seas and oceans change the amount of carbon dioxide?

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.


What gas in the atmosphere was absorbed by the oceans as they formed?

The ocean water absorbed much of the carbon dioxide from the atmosphere.


Carbon dioxide is removed 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.