Articles | Volume 15, issue 6
https://doi.org/10.5194/tc-15-3007-2021
https://doi.org/10.5194/tc-15-3007-2021
Brief communication
 | 
29 Jun 2021
Brief communication |  | 29 Jun 2021

Brief communication: Growth and decay of an ice stupa in alpine conditions – a simple model driven by energy-flux observations over a glacier surface

Johannes Oerlemans, Suryanarayanan Balasubramanian, Conradin Clavuot, and Felix Keller

Download

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on tc-2021-54', Jonathan D Mackay, 08 Apr 2021
    • AC1: 'Reply on RC1', Johannes Oerlemans, 08 May 2021
  • RC2: 'Comment on tc-2021-54', Anonymous Referee #2, 16 Apr 2021
    • AC2: 'Reply on RC2', Johannes Oerlemans, 08 May 2021
  • RC3: 'Comment on tc-2021-54', Anonymous Referee #3, 06 May 2021
    • AC3: 'Reply on RC3', Johannes Oerlemans, 08 May 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Publish subject to minor revisions (review by editor) (28 May 2021) by Chris Derksen
AR by Johannes Oerlemans on behalf of the Authors (30 May 2021)  Author's response   Manuscript 
EF by Sarah Buchmann (04 Jun 2021)  Author's tracked changes 
ED: Publish as is (04 Jun 2021) by Chris Derksen
AR by Johannes Oerlemans on behalf of the Authors (07 Jun 2021)
Download
Short summary
An ice stupa is a cone-like ice mass storing water in the form of ice. By sprinkling water on the cone during cold conditions an ice stupa can grow to achieve an appreciable mass (typically 1 × 106 kg) and release this in spring and summer in the form of meltwater. In Ladakh ice stupas are currently used more and more for irrigation purposes. We present a simple model with which the rate of growth and decay of a stupa can be calculated for given climatic conditions.