reaching Earth’s floor is increased proportionately. Ozone molecules within the stratosphere and in the troposphere absorb UV-B radiation, thereby significantly lowering the quantity that reaches Earth’s floor (see Q2). Though HCl doesn’t react directly with ozone, stratospheric injections of HCl and different chlorine-containing gases following explosive volcanic eruptions can lead, by way of chemical reactions, to elevated chlorine monoxide (ClO) that destroys ozone (see Figure Q7-3).Chemical reactions on the surface of sulfate aerosol particles destroy stratospheric ozone by growing the abundance of chlorine monoxide (ClO), a highly reactive chlorine fuel (see Q7). Finally, will increase in greenhouse gases (GHGs) similar to carbon dioxide (CO2), which warm
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