Antarctic Sea Ice and Snow Microbial Bromocarbon Processes
Naturally produced brominated organic compounds are ubiquitous in the oceans and are thought to be largely responsible for the formation of the Antarctic “ozone hole” in Spring. In order to accurately model and forecast global ozone and the climate, it is critical to include reactive bromine and brominated organic compounds (bromocarbons). However, bromocarbon measurements for the Antarctic are limited, especially during Spring.
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