Understanding the global effect of secondary organic aerosol on size distributions in past and present climates
Recent research has shown that secondary organic aerosols (SOA) are major contributors to ultrafine particle growth to climatically relevant sizes, increasing global cloud condensation nuclei (CCN) concentrations within the continental boundary layer (BL). This thesis contains two separate studies i...
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Language: | en |
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2013
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Online Access: | http://hdl.handle.net/10222/42668 |