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How will SOA change in the future?
Author(s) -
Lin Guangxing,
Penner Joyce E.,
Zhou Cheng
Publication year - 2016
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1002/2015gl067137
Subject(s) - climate change , isoprene , environmental science , global change , representative concentration pathways , earth system science , atmospheric sciences , land use, land use change and forestry , earth's energy budget , northern hemisphere , aerosol , climatology , climate model , land use , meteorology , geology , chemistry , geography , ecology , oceanography , physics , organic chemistry , quantum mechanics , radiation , copolymer , biology , polymer
Secondary organic aerosol (SOA) plays a significant role in the Earth system by altering its radiative balance. Here we use an Earth system model coupled with an explicit SOA formation module to estimate the response of SOA concentrations to changes in climate, anthropogenic emissions, and human land use in the future. We find that climate change is the major driver for SOA change under the representative concentration pathways for the 8.5 future scenario. Climate change increases isoprene emission rate by 18% with the effect of temperature increases outweighing that of the CO 2 inhibition effect. Annual mean global SOA mass is increased by 25% as a result of climate change. However, anthropogenic emissions and land use change decrease SOA. The net effect is that future global SOA burden in 2100 is nearly the same as that of the present day. The SOA concentrations over the Northern Hemisphere are predicted to decline in the future due to the control of sulfur emissions.