Cloud Condensation Nuclei in FIRE III
Yum and Hudson showed that the springtime Arctic aerosol is probably a result of long-range transport at high altitudes. Scavenging of particles by clouds reduces the low level concentrations by a factor of 3. This produces a vertical gradient in particle concentrations when low-level clouds are pre...
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Language: | unknown |
Published: |
2002
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Online Access: | http://hdl.handle.net/2060/20020076393 |