Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
6344190 | Atmospheric Research | 2010 | 6 Pages |
Abstract
Within non-precipitating clouds, total ionic content (TIC) of cloud droplets decreases with increasing liquid water content (LWC). However, this is not a simple inverse relationship. Instead, TIC has an exponential distribution with a parameter that is dependent on LWC. We demonstrate this finding using a long-term monitoring record (1994-2006) of cloud water chemistry measurements collected at the summit of Whiteface Mountain, NY.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Atmospheric Science
Authors
Nenad Aleksic, James E. Dukett,