Volcanoes Vs. Humans: Who Pollutes More?

do volcanoes put out more pollution than man

It is a common misconception that volcanic eruptions produce more pollution than human activity. While volcanoes can have a significant impact on the climate, releasing huge amounts of volcanic gas, aerosol droplets, and ash into the stratosphere, human activities emit far more carbon dioxide each year. According to the U.S. Geological Survey, volcanoes produce about 200 million tons of carbon dioxide annually, while human activities emit 24 billion tons of CO2 worldwide each year. Large volcanic eruptions may match human emissions for a few hours, but they are too rare to rival humanity's annual emissions.

Characteristics Values
Annual carbon dioxide emissions from volcanoes 0.6 billion metric tons, according to Michael Burton, Georgina Sawyer, and Domenico Granieri (2013) 200 million tons, according to the U.S. Geological Survey
Annual carbon dioxide emissions from human activity 24 billion tons, according to the U.S. Geological Survey 35 billion tons, according to the Carbon Dioxide Information Analysis Center (2010) 40 billion tons, according to the Global Carbon Project (2015)
Ratio of human to volcanic carbon dioxide emissions 60-150 times more
Impact on climate change Volcanic carbon dioxide emissions have not caused detectable global warming.
Human emissions are responsible for global warming and climate change.

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Human activities emit 60 times more carbon dioxide than volcanoes each year

According to the U.S. Geological Survey, volcanoes on land and underwater generate approximately 200 million tons of carbon dioxide annually. In contrast, human activities, such as automotive and industrial operations, are responsible for about 24 billion tons of carbon dioxide emissions per year. This discrepancy in emission levels indicates that human activities contribute significantly more to carbon dioxide levels in the atmosphere than volcanic activity.

The impact of human emissions is further highlighted by the consistent rise in atmospheric CO2 levels, regardless of volcanic eruptions in specific years. If volcanic eruptions were the primary driver of increasing carbon dioxide concentrations, we would expect to see spikes in carbon dioxide records corresponding to these events. However, the data does not support this hypothesis.

While large and violent volcanic eruptions can match the rate of human emissions during their brief duration, they are too infrequent to rival humanity's annual emissions. Additionally, several individual U.S. states emit more carbon dioxide in a year than all the volcanoes on Earth combined. This comparison underscores the significant contribution of human activities to carbon dioxide emissions.

Furthermore, estimates of carbon dioxide emissions from Mount Etna, Europe's most active volcano, range from 3 million tons per year to 10,000 times less than mankind's total emissions. These estimates further emphasize the disparity between volcanic and human-induced carbon dioxide emissions.

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Volcanic eruptions can cause global cooling, while carbon dioxide emissions from volcanoes can cause global warming

Volcanic eruptions can have a profound impact on the climate, causing both global cooling and warming. During eruptions, volcanoes release vast amounts of volcanic gases, aerosol droplets, and ash into the stratosphere. While the ash and aerosol droplets can cause global cooling, the volcanic gases, including carbon dioxide, contribute to global warming.

The cooling effect of volcanic eruptions is primarily due to the ash and aerosol droplets, such as sulfur dioxide, that are injected into the stratosphere. These particles and droplets reflect and block incoming solar radiation, leading to a temporary cooling effect that can last from months to years, depending on the eruption's magnitude. The sulfur dioxide combines with water vapour to form sulfuric acid aerosols, which remain in the stratosphere for up to three years, causing significant cooling worldwide.

On the other hand, volcanoes also emit substantial amounts of carbon dioxide, a potent greenhouse gas. While the amount of carbon dioxide released during a single eruption can be significant, it is the cumulative effect of constant human emissions from burning fossil fuels that far outweighs volcanic emissions over time. Human activities emit 60 or more times the amount of carbon dioxide released by volcanoes annually, with certain individual US states emitting more carbon dioxide than all volcanoes combined.

Volcanoes emit carbon dioxide not only during eruptions but also through underground magma. The degassing of subterranean magma when a volcano is not erupting contributes significantly to volcanic carbon dioxide emissions. While volcanic carbon dioxide emissions estimates range from 0.13 to 0.6 billion metric tons per year, human emissions are significantly higher, reaching 35 billion metric tons per year from fossil fuels and cement production alone.

Therefore, while volcanic eruptions can cause short-term global cooling through the release of ash and aerosols, the carbon dioxide and other greenhouse gases emitted contribute to the long-term global warming trend, especially when combined with human-induced emissions.

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The largest volcanic eruptions emit 10-50 million tons of carbon dioxide, while human activities emit 24 billion tons of CO2 annually

The debate about whether volcanoes or human activities contribute more to climate change has been ongoing for years. While volcanoes emit carbon dioxide and other greenhouse gases that can cause global warming, human activities, such as burning fossil fuels and deforestation, are the major drivers of climate change.

According to the provided statement, the largest volcanic eruptions can emit between 10 and 50 million tons of carbon dioxide. This is indeed a significant amount, and large eruptions can impact the climate. For example, the 1980 eruption of Mount St. Helens released approximately 10 million tons of carbon dioxide in just 9 hours. Similarly, the 1991 eruption of Mount Pinatubo, one of the largest of the twentieth century, injected a 20-million-ton sulfur dioxide cloud into the stratosphere.

However, these large volcanic eruptions are relatively rare and fleeting. In contrast, human activities emit carbon dioxide continuously and at a much larger scale. According to the U.S. Geological Survey, human activities, such as automotive and industrial processes, emit about 24 billion tons of carbon dioxide annually. This is several times higher than the estimated global volcanic carbon dioxide emissions, which range from 0.13 to 0.44 gigatons per year, with a more conservative estimate of 0.6 billion metric tons per year.

The impact of human activities on the atmosphere is further highlighted by the consistent rise in atmospheric CO2 levels, regardless of whether there are major volcanic eruptions in specific years. If volcanic eruptions were the primary cause of increasing carbon dioxide concentrations, we would expect to see spikes in the carbon dioxide records for each significant eruption. Instead, human activities have added more than 2,000 billion metric tons of carbon dioxide to the atmosphere since the Industrial Revolution.

In summary, while volcanoes can emit significant amounts of carbon dioxide during large eruptions, human activities are responsible for much higher emissions on an annual basis. The cumulative effect of human activities has led to a continuous rise in atmospheric CO2 levels, contributing to climate change. Therefore, addressing human-induced emissions is crucial in mitigating the impact on our planet's climate.

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Volcanic carbon dioxide emissions are released during eruptions and through underground magma

Volcanoes emit carbon dioxide in two ways: during eruptions and through underground magma. Carbon dioxide from underground magma is released through vents, porous rocks and soils, and water that feeds volcanic lakes and hot springs. Much of the carbon dioxide released by volcanoes is emitted by the degassing of subterranean magma when the volcano is not erupting.

The 1980 eruption of Mount St. Helens, for example, vented approximately 10 million tons of carbon dioxide into the atmosphere in just nine hours. However, such massive eruptions are rare and fleeting. Large, violent eruptions may match the rate of human emissions for a few hours, but they are too infrequent to rival humanity's annual emissions.

According to the U.S. Geological Survey, the world's volcanoes generate about 200 million tons of carbon dioxide annually. In comparison, human activities, primarily the burning of fossil fuels, emitted roughly 40 billion metric tons of carbon dioxide in 2015. Since the start of the Industrial Revolution, human emissions of carbon dioxide have risen to more than 35 billion metric tons per year, while volcanoes produce less than 1 billion metric tons annually.

While volcanic activity has contributed to global warming over geological time by producing significant amounts of carbon dioxide, current volcanic activity does not occur on the same massive scale. Today, human emissions far outweigh volcanic emissions, and atmospheric carbon dioxide levels have consistently risen year after year, regardless of whether there have been major volcanic eruptions.

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Volcanic activity contributes to melting Antarctica's ice sheets from below, while human-induced emissions erode them from above

While human activities emit 60 or more times the amount of carbon dioxide released by volcanoes annually, volcanic activity contributes to melting Antarctica's ice sheets from below. Scientists Hugh Corr and David Vaughan of the British Antarctic Survey believe that volcanoes underneath Antarctica may be melting the continent's ice sheets from below, just as human-induced emissions erode them from above. Corr and Vaughan's theory is supported by the discovery of volcanic ash in ice cores from West Antarctica, which indicates the presence of past volcanic activity.

Further evidence for the role of volcanic activity in melting Antarctica's ice sheets comes from a 2018 study published in Nature Communications. In this study, researchers measured the composition of isotopes of helium detected in glacial meltwater flowing from the Pine Island Glacier Ice Shelf, the fastest-melting glacier in Antarctica. The results suggested the presence of a volcanic heat source upstream of the ice shelf, which may be triggering melting beneath the glacier.

While volcanic activity may contribute to the melting of Antarctica's ice sheets, human-induced emissions are also a significant factor. A study by U.S. and U.K. scientists found the first evidence of a direct link between human-induced climate change and the melting of the West Antarctic Ice Sheet. The researchers combined satellite observations and climate model simulations to understand how winds over the ocean near West Antarctica have changed since the 1920s in response to rising greenhouse gas concentrations. They found that human-induced climate change has caused a long-term change in the winds, leading to more prevalent warm ocean conditions that contribute to ice melt.

In addition to the direct impact of human-induced emissions on Antarctica's ice sheets, there is also an indirect effect. As the ice sheets melt, the land underneath lifts slightly due to the reduction in weight, a process called isostatic rebound. This can push magma upward, causing volcanic eruptions that further melt the ice above. This creates a cycle that speeds up ice loss and sea-level rise.

Overall, while volcanic activity may contribute to the melting of Antarctica's ice sheets from below, human-induced emissions are a more significant factor in eroding the ice sheets from above. Human activities emit much higher levels of carbon dioxide than volcanoes, and the impact of these emissions on the climate is driving the melting of Antarctica's ice sheets.

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Frequently asked questions

No. While volcanic eruptions can inject significant amounts of carbon dioxide into the atmosphere, human activities emit 60 or more times the amount of carbon dioxide released by volcanoes annually.

Published scientific estimates of the global CO2 emission rate for all degassing subaerial and submarine volcanoes range from 0.13 to 0.44 gigatons per year. However, some estimates place this figure at 200 million tons of carbon dioxide per year.

Yes, volcanic eruptions can impact climate change. During major eruptions, huge amounts of volcanic gases, aerosol droplets, and ash are injected into the stratosphere. While the injected ash falls rapidly from the stratosphere and has little impact on climate change, volcanic gases like sulfur dioxide can cause global cooling, while volcanic carbon dioxide, a greenhouse gas, can promote global warming.

Human activities that contribute to carbon dioxide emissions include the burning of fossil fuels, cement production, deforestation, and other landscape changes.

Mount St. Helens, Pinatubo, Laki, Krakatau, and Tambora have all had significant impacts on the climate in recent history. For example, the 1980 eruption of Mount St. Helens released approximately 10 million tons of carbon dioxide into the atmosphere in just 9 hours, while the 1991 eruption of Mount Pinatubo injected a 20-million-ton sulfur dioxide cloud into the stratosphere.

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