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Ik
The oceans play an important role in regulating the amount of CO 2 in the atmosphere because CO 2 can move quickly into and out of the oceans. Once in the oceans, the CO 2 no longer traps heat. CO 2 also moves quickly between the atmosphere and the land biosphere (material that is or was living on land).Of the three places where carbon is stored---atmosphere, oceans, and land biosphere---approximately 93 percent of the CO 2 is found in the oceans. The atmosphere, at about 750 petagrams of carbon (a petagram [Pg] is 10 15 grams), has the smallest amount of carbon
Too much carbon dioxide in the atmosphere is causing global warming. The natural carbon cycle is overwhelmed and can't move out all the extra gas. The extra gas is turning the natural greenhouse effect into an accelerated greenhouse effect, which is causing global warming.
The cycle that move and recycles water in its various forms through the biosphere is called the water cycle. The water cycle is a constant process.
The usage of non renewable sources of energy are causing the greenhouse effect. The energy sources such as coal, oil, and natural gases omit carbon dioxide into the atmosphere, causing the greenhouse effect.
Ik
photosynthesis: plants take in carbon dioxide during photosynthesis and use it to build carbohydrates.dissolving: carbon dioxide dissolves in rainwater and oceans.
Plants absorb carbon dioxide from the atmosphere.
The oceans play an important role in regulating the amount of CO 2 in the atmosphere because CO 2 can move quickly into and out of the oceans. Once in the oceans, the CO 2 no longer traps heat. CO 2 also moves quickly between the atmosphere and the land biosphere (material that is or was living on land).Of the three places where carbon is stored---atmosphere, oceans, and land biosphere---approximately 93 percent of the CO 2 is found in the oceans. The atmosphere, at about 750 petagrams of carbon (a petagram [Pg] is 10 15 grams), has the smallest amount of carbon
the carbon dissolves into the water
The oceans, and other bodies of water, soak up some carbon from the atmosphere.
Respiration, then travels to the biotic part of the biosphere(through trees, etc.)
Earth's systems interact through processes like the carbon cycle, water cycle, and nutrient cycling. For example, the atmosphere and hydrosphere interact through precipitation and evaporation, while the biosphere interacts with the geosphere through processes like weathering and soil formation. These interactions are essential for maintaining Earth's delicate balance and supporting life.
The biosphere serves as an interface between the spheres, enabling water to move between the lithosphere, hydrosphere, and atmosphere.
The oxygen moves through the biosphere as a part of the carbon cycle by breeding and attaching within the bodies exporital fluid system. Scientists to not know yet what is the real reason but we assume that a masterbating scientist may have the answer just ask the teacher that masterbates.
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Given off by animals as a waste product. Used by plants to maintain life. nova net Carbon dioxide (CO2) is considered a trace gas in the atmosphere because it is much less abundant than oxygen or nitrogen. However, this trace gas plays a vital role in sustaining life on Earth and in controlling the Earth's climate by trapping heat in the atmosphere. The oceans play an important role in regulating the amount of CO2in the atmosphere because CO2 can move quickly into and out of the oceans. Once in the oceans, the CO2 no longer traps heat. CO2 also moves quickly between the atmosphere and the land biosphere (material that is or was living on land). Of the three places where carbon is stored-atmosphere, oceans, and land biosphere-approximately 93 percent of the CO2 is found in the oceans. The atmosphere, at about 750 petagrams of carbon (a petagram [Pg] is 1*10^15 grams), has the smallest amount of carbon. Approximately 90 to 100 Pg of carbon moves back and forth between the atmosphere and the oceans, and between the atmosphere and the land biosphere. Although these exchange rates are large relative to the total amount of carbon stored in the atmosphere, the concentration of CO2 was constant at 280 parts per million (ppm) by volume for at least 1,000 years prior to the industrial era. Atmospheric concentrations of CO2 were constant because the carbon being removed from the atmosphere in some places exactly matched the CO2 being added to the atmosphere in other places. Marine plants and animals play a role in the uptake and release of carbon dioxide in the ocean. Plants, primarily phytoplankton but also macrophytes such as this seaweed, take up carbon dioxide and release oxygen, which oxygen-dependent animals need to survive.