Articles | Volume 13, issue 1
https://doi.org/10.5194/tc-13-219-2019
https://doi.org/10.5194/tc-13-219-2019
Research article
 | 
24 Jan 2019
Research article |  | 24 Jan 2019

Characterizing the behaviour of surge- and non-surge-type glaciers in the Kingata Mountains, eastern Pamir, from 1999 to 2016

Mingyang Lv, Huadong Guo, Xiancai Lu, Guang Liu, Shiyong Yan, Zhixing Ruan, Yixing Ding, and Duncan J. Quincey

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 Guang Liu on behalf of the Authors (13 Oct 2018)  Author's response   Manuscript 
ED: Reconsider after major revisions (30 Oct 2018) by Arjen Stroeven
AR by Guang Liu on behalf of the Authors (01 Nov 2018)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (06 Nov 2018) by Arjen Stroeven
RR by Luke Copland (03 Dec 2018)
ED: Publish subject to technical corrections (10 Jan 2019) by Arjen Stroeven
AR by Guang Liu on behalf of the Authors (17 Jan 2019)  Author's response   Manuscript 
Download
Short summary
We highlight 28 glaciers in the Kingata Mountains, among which 17 have changed markedly over the last decade. We identify four advancing and 13 surge-type glaciers. The dynamic evolution of the surges is similar to that of Karakoram, suggesting that both hydrological and thermal controls are important for surge initiation and recession. Topography seems to be a dominant control on non-surge glacier behaviour. Most glaciers experienced a significant and diverse change in their motion patterns.