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Aerosol size distribution and radiative forcing response to anthropogenically driven historical changes in biogenic secondary organic aerosol formation

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Academic year: 2017

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Figure 1. Absolute change in (a) isoprene, (c) monoterpene, and (e) sesquiterpene emissions between the years 1000–1010 and 1980–1990 in mg m −2 day −1 from the MEGAN terpenoid reconstruction, and absolute change in (b) isoprene, and (d) monoterpene emissi
Table 1. Summary of the GEOS-Chem-TOMAS simulations performed in this study. Biogenic emissions for year 1000 and 2000 using MEGAN are decadal-averaged emissions for 1000–1010 and 1980–1990, respectively, whereas LPJ-GUESS biogenic emissions are  annual-av
Figure 2. Mean millennial fixed-yield biogenic SOA formation from (a) MEGAN emissions and (b) LPJ-GUESS emissions between the periods 1000–2000 in mg m − 2 day − 1
Figure 3. Percent contribution to SOA formation by (a) iso- iso-prene, (b) monoterpene, and (c) sesquiterpene emissions from the MEGAN reconstruction, averaged over the years 1000–2000
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