Abstract
We address theoretically the longstanding problem of particle dispersion in the lower atmosphere. The evolution of particle concentration under an absorbing boundary condition at the ground is described. We derive a close-form solution for the downwind surface density of deposited particles and find how the number of airborne particles decreases with time. The problem of the plume formation above the extended surface source is also solved analytically. At the end, we show how turbophoresis modifies the mean settling velocity of particles.
Original language | English |
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Pages (from-to) | 23-40 |
Number of pages | 18 |
Journal | Boundary-Layer Meteorology |
Volume | 159 |
Early online date | 12 Nov 2015 |
DOIs | |
State | Published - Apr 2016 |
All Science Journal Classification (ASJC) codes
- Atmospheric Science