Scavenging calculation
Particles are scavenged by cloud droplets in the cloud, and by falling raindrops below the cloud. The change in concentration C is described by the exponential relation C=C0 exp (- λt)
In-cloud scavenging Below-cloud scavenging |
The in-cloud scavenging coefficient λicp and below-cloud scavenging coefficient λbcp depend on dd drop diameter Ec collection efficiency for precipitating cloud droplets Ep collection efficiency for particles P precipitation rate in mm/hr (at ground level) |
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The net change of concentration can be calculated straightforwardly when using these parameterizations. However, the collection efficiencies themselves are a function of droplet size and particle size distribution.
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Read also |
Visit the NanoFASE Library for abstracts of deliverable reports. |
Seinfeld, J. H., & Pandis, S. N. (2016). Atmospheric Chemistry and Physics, Wiley-Inter Science, Chapter 20 pp 856-859. |
Contact
Astrid Manders
TNO, Netherlands