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Volcanic Eruptions and the Atmosphere

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In what ways do the volcanic gases from volcanic eruptions develop the atmosphere? When a volcano erupts, a plethora of debris and other hazards flows out from the mouth of the volcano. Of this debris, one of the most perilous threats is not only the lava but also any gases that are a product of the eruption. In fact, these gases that are released during, after, and sometimes before an eruption are one of the main culprits as to why volcanos erupt. These gases include, but are not limited to: sulfur dioxide (SO2), hydrogen sulfide (H2S), carbon dioxide (CO2), hydrogen chloride (HCl), and hydrogen fluoride (HF). These gases are the cause of several devastating phenomenon that are widely known to affect the atmosphere: the haze effect, the depletion of the Ozone layer, and global warming related to the emission of greenhouse gases.
The haze effect is defined as when “Suspended particles, such as dust and ash…block out the earth's sunlight, thus reducing solar radiation and lowering mean global temperatures.”( http://www.geology.sdsu.edu/how_volcanoes_work/climate_effects.html) While this statement holds true, it was found that it was not only the dust particles that caused lowering mean global temperatures, but it was also the discharge of sulfuric-rich gases; the main gas being SO2. According to the U.S. Geological Survey (USGS), “Emission rates of SO2 from an active volcano range from <20 tonnes/day to >10 million tonnes/day...”

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