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Non-volatile residuals of newly formed atmospheric particles in the boreal forest

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Academic year: 2021

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Figure

Table 1. Time differences between the detection of new particles and their cores, and the corresponding growth rates.
Fig. 1. Transport efficiency of a TSI3025 CPC and the heating tube (at 280 ◦ C) used in the V-SMPS setup as a function of particle size
Fig. 2. The particle number size distribution during 26–27 March 2006. The top figure shows the DMPS data, the middle figure the ambient SMPS data, and the bottom figure the heated SMPS data.
Fig. 3. The particle concentrations measured with the DMPS, and the heated and non-heated SMPS.
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