Articles | Volume 18, issue 24
Atmos. Chem. Phys., 18, 18063–18078, 2018
https://doi.org/10.5194/acp-18-18063-2018
Atmos. Chem. Phys., 18, 18063–18078, 2018
https://doi.org/10.5194/acp-18-18063-2018

Research article 20 Dec 2018

Research article | 20 Dec 2018

Spatial and temporal changes in SO2 regimes over China in the recent decade and the driving mechanism

Ting Wang et al.

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Ting Wang on behalf of the Authors (24 Oct 2018)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (09 Nov 2018) by Dominick Spracklen
RR by Anonymous Referee #1 (21 Nov 2018)
RR by Anonymous Referee #2 (29 Nov 2018)
ED: Publish subject to technical corrections (30 Nov 2018) by Dominick Spracklen
AR by Ting Wang on behalf of the Authors (03 Dec 2018)  Author's response    Manuscript
Download
Short summary
In the last decade, four temporal regimes of SO2 in China have been identified. After an initial rise, SO2 undergoes two sharp drops in 2007–2008 and 2014–2016, during which 5-year rebounding is sustained. Different mechanisms are tied to North and South China. The industrial emission is responsible for SO2 variation in North China, while in South China the meteorological conditions make a large contribution. The result is crucial to the understanding of SO2 changes and future polices.
Altmetrics
Final-revised paper
Preprint