RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 17, ES4001, doi:10.2205/2017ES000604, 2017
Figure 6. Time evolution of the particle size spectrum. No protoaerosol has presented before the source began to produce fresh particles. But in contrast to Figure 3 the source stops to work at 7 a.m.. The aerosols formed by the source until this time begins to grow. The picture reminds that shown in Figure 4.
Citation: Lushnikov A. A., V. A. Zagaynov, Yu. S. Lyubovtseva (2017), Formation of aerosols in the lower troposphere, Russ. J. Earth Sci., 17, ES4001, doi:10.2205/2017ES000604.
Copyright 2017 by the Geophysical Center RAS.
Generated from LaTeX source by ELXpaper, v.1.5 software package.