The Cryosphere
The Cryosphere
TC
Articles | Volume 15, issue 6
Articles | Volume 15, issue 6
https://doi.org/10.5194/tc-15-3007-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-15-3007-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 15, issue 6
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

Viewed

Total article views: 2,359 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,382 922 55 2,359 38 43
  • HTML: 1,382
  • PDF: 922
  • XML: 55
  • Total: 2,359
  • BibTeX: 38
  • EndNote: 43
Views and downloads (calculated since 01 Apr 2021)
Cumulative views and downloads (calculated since 01 Apr 2021)

Viewed (geographical distribution)

Total article views: 2,359 (including HTML, PDF, and XML) Thereof 2,280 with geography defined and 79 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 25 Apr 2024
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.
Read more