Earth has many processes that regulate carbon, atmospheric carbon dioxide and its role in the carbon cycle and climate. How much do you know?
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Using NASA satellites such as Landsat, people can study the severity, size and location of forest fires from space, and we can estimate how much carbon is released into the atmosphere as the fires burn.
Plants such as trees, grasses and crops that are photosynthesizing reflect strongly in infrared light (light with wavelengths longer than those of visible light). We cannot see infrared light, but instruments on satellites like the Landsat satellite can. By precisely measuring the amount of infrared light reflected by plants, we can get a handle on the health of that vegetation.
Collectively, the entire human race breathes out about 2000 lbs of carbon dioxide (roughly 1 metric ton) per day. With about seven billion humans on Earth, we collectively release about 7 billion kilograms (7 million metric tons) of carbon dioxide each day into the atmosphere. However, this does not contribute to the build-up of carbon dioxide in our atmosphere that we are seeing because all the carbon in our body comes either directly or indirectly from plants, and those plants took it out of the air only recently. When we breathe out, all the carbon dioxide we exhale has already been accounted for. By breathing out, we are simply returning to the air the same carbon that was there to begin with. This is why it's called a "carbon cycle."
The surface of the oceans both releases carbon dioxide into the air and absorbs or stores it. One-third of all carbon dioxide emitted by humanity has been absorbed by the world’s oceans. This is making them more acidic than they have been for tens of millions of years. More acidic seawater has negative effects on coral reefs, slowing their growth and bleaching them. A more acidic ocean is affecting plankton (which provide half of the oxygen we breathe) and many marine organisms. Due to global warming, the capacity to provide oxygen and support the food chains of the ocean has fallen by 6 percent over the last 30 years. In addition, as the oceans get warmer (as the result of global warming), they are less able to store carbon; they therefore emit more carbon dioxide back into the atmosphere where it causes further warming.
Oxygen has an atomic mass of 16 while carbon has an atomic mass of 12. The atomic mass of an element is the average mass of the protons, neutrons and electrons in an atom of that element when it is at rest.
In contrast to the Northern Hemisphere, the Southern Hemisphere is covered by more ocean than vegetation.
The idea of global warming goes back to the Victorians. In 1896, Svante Arrhenius published a paper that was the first to measure how carbon dioxide contributes to the greenhouse effect. Carbon dioxide warms the Earth by trapping heat near the surface, a bit like swaddling the planet in an extra blanket. Arrhenius was also the first to speculate about whether changes in the amount of carbon dioxide in the atmosphere have contributed to long-term variations in Earth’s climate. He later made the link between burning fossil fuels and global warming, a link we are clearly seeing today.
Carbon dioxide is not the only carbon-containing compound in the atmosphere that affects our climate. Methane (which comes from livestock, leakage from natural gas systems and wetlands) is a potent heat-trapping greenhouse gas. Carbon monoxide (which comes from unvented heaters and generators and other gasoline-powered equipment) affects methane, carbon dioxide and ozone levels in the atmosphere. Because carbon monoxide lingers in the air for about a month it can travel long distances, making it useful for studying how air pollution moves around the world. Black carbon (soot) is the byproduct of burning fuels like petroleum and coal. When black carbon settles on ice and snow in the Arctic and Antarctic or on mountain glaciers it darkens the surface of the snow, speeding up melt and reducing freshwater availability.
Every time we drive a car, take a flight or cut down trees or clear land of vegetation, we add carbon dioxide into the atmosphere.
Plants have taken up about a quarter, not half, of the carbon dioxide we've pumped into our air over the last several decades. When plants have enough water and nitrogen, they tend to grow more if there is a lot of carbon dioxide in the air. As we add more carbon dioxide to the air (through burning of fossil fuels, cutting down trees and so on), the possible additional growth by vegetation may help counter some of our impacts. However, we may not be able to count on plants to continue to take up extra carbon dioxide, because plants have limits to the amount they can grow. In addition, as the planet warms (a result of our carbon emissions), we will see more drought in many places, and this will affect the amount of water available for plants’ growth.