Articles | Volume 12, issue 1
https://doi.org/10.5194/tc-12-95-2018
https://doi.org/10.5194/tc-12-95-2018
Brief communication
 | 
11 Jan 2018
Brief communication |  | 11 Jan 2018

Brief communication: The Khurdopin glacier surge revisited – extreme flow velocities and formation of a dammed lake in 2017

Jakob F. Steiner, Philip D. A. Kraaijenbrink, Sergiu G. Jiduc, and Walter W. Immerzeel

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 Jakob F. Steiner on behalf of the Authors (11 Oct 2017)  Author's response   Manuscript 
ED: Publish subject to minor revisions (Editor review) (17 Oct 2017) by Olaf Eisen
AR by Jakob F. Steiner on behalf of the Authors (21 Nov 2017)  Author's response   Manuscript 
ED: Publish subject to technical corrections (26 Nov 2017) by Olaf Eisen
AR by Jakob F. Steiner on behalf of the Authors (26 Nov 2017)  Author's response   Manuscript 
Download
Short summary
Glaciers that once every few years or decades suddenly advance in length – also known as surging glaciers – are found in many glaciated regions in the world. In the Karakoram glacier tongues are additionally located at low altitudes and relatively close to human settlements. We investigate a very recent and extremely rapid surge in the region that has caused a lake to form in the main valley with possible risks for downstream communities.