Articles | Volume 17, issue 3
https://doi.org/10.5194/nhess-17-345-2017
https://doi.org/10.5194/nhess-17-345-2017
Research article
 | 
08 Mar 2017
Research article |  | 08 Mar 2017

Meteorological factors driving glacial till variation and the associated periglacial debris flows in Tianmo Valley, south-eastern Tibetan Plateau

Mingfeng Deng, Ningsheng Chen, and Mei Liu

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Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (further review by Editor and Referees) (18 Nov 2016) by Paolo Tarolli
AR by Mingfeng Deng on behalf of the Authors (20 Nov 2016)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (25 Nov 2016) by Paolo Tarolli
RR by Anonymous Referee #2 (02 Dec 2016)
RR by Francesco Comiti (22 Dec 2016)
ED: Reconsider after major revisions (further review by Editor and Referees) (10 Jan 2017) by Paolo Tarolli
AR by Mingfeng Deng on behalf of the Authors (13 Jan 2017)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (15 Jan 2017) by Paolo Tarolli
RR by Anonymous Referee #2 (19 Jan 2017)
ED: Publish subject to minor revisions (further review by Editor) (24 Jan 2017) by Paolo Tarolli
AR by Mingfeng Deng on behalf of the Authors (28 Jan 2017)  Author's response    Manuscript
ED: Publish as is (19 Feb 2017) by Paolo Tarolli
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Short summary
Annual air temperature spiked and glacier retreated shortly before the three periglacial debris flows in Tianmo valley. However, they did not occur when glacier retreat was sharpest, resulting from the frozen bared glacial till as the melting of internal ice lags behind glacial retreat. The activity of the glacial till can be enhanced by prolonged high air temperature. Finally, either rainfall or continuous percolation of ice ablation water flows can generate debris flow.
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