Articles | Volume 15, issue 23
Atmos. Chem. Phys., 15, 13777–13786, 2015
https://doi.org/10.5194/acp-15-13777-2015
Atmos. Chem. Phys., 15, 13777–13786, 2015
https://doi.org/10.5194/acp-15-13777-2015

Research article 15 Dec 2015

Research article | 15 Dec 2015

Role of radiatively forced temperature changes in enhanced semi-arid warming in the cold season over east Asia

X. Guan et al.

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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Jianping Huang on behalf of the Authors (31 Oct 2015)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (03 Nov 2015) by Hailong Wang
RR by Anonymous Referee #1 (23 Nov 2015)
ED: Reconsider after minor revisions (Editor review) (25 Nov 2015) by Hailong Wang
AR by Jianping Huang on behalf of the Authors (28 Nov 2015)  Author's response    Manuscript
ED: Publish as is (04 Dec 2015) by Hailong Wang
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Short summary
Dynamical adjustment methodology has been applied to the raw surface air temperature and has successfully identified and separated the contribution of dynamically induced temperature (DIT) and radiatively forced temperature (RFT). It found that regional anthropogenic radiative forcing caused the enhanced warming in the semi-arid region, which may be closely associated with local human activities.
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