Climate Change - Aerosols in the
        Stratosphere 
        
            Largely injected
                by volcanic eruptions 
             
            remember, the
                stratosphere is a stable layer, so lighter,
                smaller aerosols will have long residence times 
             
            aerosols reflect
                and absorb short wave radiation 
             
            As a result
                aerosols produce warming in the stratosphere and
                cooling in the troposphere  
             
            Recent significant
                eruptions: 
                
             
         
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