Glacier melting and precipitation trends detected by surface area
changes in Himalayan ponds

Salerno, Franco; Thakuri, Sudeep; Guyennon, Nicolas; Viviano, Gaetano; Tartari, Gianni

doi:https://doi.org/10.5194/tc-10-1433-2016

Articles | Volume 10, issue 4

https://doi.org/10.5194/tc-10-1433-2016

© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

https://doi.org/10.5194/tc-10-1433-2016

© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 10, issue 4

Research article

|

11 Jul 2016

Research article |

| 11 Jul 2016

Glacier melting and precipitation trends detected by surface area changes in Himalayan ponds

Franco Salerno, Sudeep Thakuri, Nicolas Guyennon, Gaetano Viviano, and Gianni Tartari

Download

Final revised paper (published on 11 Jul 2016)
Supplement to the final revised paper
Preprint (discussion started on 22 Mar 2016)
Supplement to the preprint

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

- Printer-friendly version

- Supplement

RC1: 'Glacier melting and precipitation trends detected by surface area changes in Himalayan ponds', Anonymous Referee #1, 28 Apr 2016
- AC2: 'Reply Rev1', Franco Salerno, 10 Jun 2016
SC1: 'Review of "Glacier melting and precipitation trends detected by surface area changes in Himalayan ponds" by Salerno et al', Argha Banerjee, 03 May 2016
- AC1: 'Reply REV1', Franco Salerno, 10 Jun 2016
RC2: 'Review', Argha Banerjee, 04 May 2016
- AC3: 'Reply REV2', Franco Salerno, 10 Jun 2016
RC3: ''Glacier melting and precipitation trends detected by surface area changes in Himalayan ponds' by Salerno et al.', Pascal Buri, 20 May 2016
- AC4: 'Reply REV3', Franco Salerno, 10 Jun 2016

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

AR by Franco Salerno on behalf of the Authors (14 Jun 2016) Author's response Manuscript

ED: Publish as is (15 Jun 2016) by G. Hilmar Gudmundsson

Short summary

This contribution shows that the surface area variations of unconnected glacial ponds, i.e. ponds not directly connected to glacier ice, can be considered as suitable proxies for detecting past changes in the main hydrological components of the water balance (glacier melt, precipitation, evaporation) on the south side of Mt Everest.