The Earth's Electrical Environment (1986) / Chapter Skim
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Pages 161-161
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From left to right are the "classical" electrode effect in clean, nonturbulent air with uniform ionization, as in Figure 11.3; the effect of aerosol attachment on the nonturbulent case; the effect of a shallow layer of high ionization rate on the nonturbulent case; and the effect of strong turbulence. Convection Currents in the Planetary Boundary Layer The downward conduction-current density is often observed to vary with altitude in the PBL.
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