Articles | Volume 17, issue 1
https://doi.org/10.5194/cp-17-241-2021
https://doi.org/10.5194/cp-17-241-2021
Research article
 | 
26 Jan 2021
Research article |  | 26 Jan 2021

The response of annual minimum temperature on the eastern central Tibetan Plateau to large volcanic eruptions over the period 1380–2014 CE

Yajun Wang, Xuemei Shao, Yong Zhang, and Mingqi Li

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
ED: Publish subject to minor revisions (review by editor) (03 Nov 2020) by Kevin Anchukaitis
AR by Yong Zhang on behalf of the Authors (13 Nov 2020)  Author's response    Manuscript
ED: Publish as is (07 Dec 2020) by Kevin Anchukaitis
Download
Short summary
It is not clear to what extent or in what manner a strong volcanic eruption will influence temperature in different regions over the long term. Therefore, new 635-year annual mean minimum temperatures (Tmin) across the eastern central Tibetan Plateau were used to explored the response of Tmin to strong volcanic eruptions. Our results show that there is a high probability that the Tmin decreases within 2 years of a large volcanic eruption, especially when such eruptions occur in low latitudes.