Analysis of information sources in references of the Wikipedia article "Ozone depletion" in English language version.
Thus, fluorine chemistry does not represent a significant sink for stratospheric ozone. All fluorine released from the source gases ends up in the form of HF, which accumulates in the stratosphere (Fig. 8). ... The high stability of HF makes it an effective tracer of fluorine input in the stratosphere arising from fluorinated anthropogenic gases
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: CS1 maint: location missing publisher (link)Thus, fluorine chemistry does not represent a significant sink for stratospheric ozone. All fluorine released from the source gases ends up in the form of HF, which accumulates in the stratosphere (Fig. 8). ... The high stability of HF makes it an effective tracer of fluorine input in the stratosphere arising from fluorinated anthropogenic gases
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: CS1 maint: numeric names: authors list (link)Free radical reactions for ozone removal: Reaction 4.1
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: CS1 maint: numeric names: authors list (link)Free radical reactions for ozone removal: Reaction 4.1
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: CS1 maint: DOI inactive as of November 2024 (link)Free radical reactions for ozone removal: Reaction 4.1
Iodine is a component of several gases that are naturally emitted from the oceans. Although iodine can participate in ozone destruction reactions, these iodine-containing source gases generally have very short lifetimes and, as a result, only a very small fraction reaches the stratosphere. There are large uncertainties in how these emissions vary with season and geographical region.
Free radical reactions for ozone removal: Reaction 4.1
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: CS1 maint: DOI inactive as of November 2024 (link)Iodine is a component of several gases that are naturally emitted from the oceans. Although iodine can participate in ozone destruction reactions, these iodine-containing source gases generally have very short lifetimes and, as a result, only a very small fraction reaches the stratosphere. There are large uncertainties in how these emissions vary with season and geographical region.
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