Introduction
Recent studies have identified important chemical processes occurring in snow and ice in polar, alpine, and midlatitude regions that can influence the chemical composition of snow/ice and the surrounding environment. Many processes are photochemically driven and can significantly impact the composition of the atmosphere overlying these chemically active snowpacks. Observations include both ozone and mercury depletion in the lower atmosphere, driven by interactions between the atmosphere and photochemically active snow/ice. These processes may also impact the overall oxidizing capacity of the tropospheric boundary layer.
Photochemical processes in snow and ice
In the mid-1980s scientists made the shocking discovery of complete ozone removal from the marine boundary layer in the Arctic. Concentrations of ozone in the lowest portion of the atmosphere were occasionally significantly depleted from typical background levels of 40 ppb (parts per billion). It was found that the...
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Grannas, A.M. (2011). Chemical Processes in Snow and Ice. In: Singh, V.P., Singh, P., Haritashya, U.K. (eds) Encyclopedia of Snow, Ice and Glaciers. Encyclopedia of Earth Sciences Series. Springer, Dordrecht. https://doi.org/10.1007/978-90-481-2642-2_625
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DOI: https://doi.org/10.1007/978-90-481-2642-2_625
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