Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
6335970 | Atmospheric Environment | 2016 | 6 Pages |
Abstract
Below-cloud scavenging coefficients for ultrafine particles (UFP) exhibit comparatively large uncertainties in part because of the limited availability of observational data sets from which robust parameterizations can be derived or that can be used to evaluate output from numerical models. Long time series of measured near-surface UFP size distributions and precipitation intensity from the Midwestern USA are used here to explore uncertainties in scavenging coefficients and test both the generalizability of a previous empirical parameterization developed using similar data from a boreal forest in Finland (Laakso et al., 2003) and whether a more parsimonious formulation can be developed. Scavenging coefficients (λ) over an ensemble of 95 rain events (with a median intensity of 1.56 mm hâ1) and 104 particle diameter (Dp) classes (from 10 to 400 nm) indicate a mean value of 3.4 Ã 10â5 sâ1 (with a standard error of 1.1 Ã 10â6 sâ1) and a median of 1.9 Ã 10â5 sâ1 (interquartile range: â2.0 Ã 10â5 to 7.5 Ã 10â5 sâ1). The median scavenging coefficients for Dp: 10-400 nm computed over all 95 rain events exhibit close agreement with the empirical parameterization proposed by (Laakso et al., 2003). They decline from â¼4.1 Ã 10â5 sâ1 for Dp of 10-19 nm, to â¼1.6 Ã 10â5 sâ1 for Dp of 80-113 nm, and show an increasing tendency for Dp > 200 nm.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Atmospheric Science
Authors
S.C. Pryor, V.M. Joerger, R.C. Sullivan,