Articles | Volume 18, issue 5
https://doi.org/10.5194/tc-18-2195-2024
https://doi.org/10.5194/tc-18-2195-2024
Research article
 | 
03 May 2024
Research article |  | 03 May 2024

Experimental modelling of the growth of tubular ice brinicles from brine flows under sea ice

Sergio Testón-Martínez, Laura M. Barge, Jan Eichler, C. Ignacio Sainz-Díaz, and Julyan H. E. Cartwright

Viewed

Total article views: 969 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
635 278 56 969 44 41
  • HTML: 635
  • PDF: 278
  • XML: 56
  • Total: 969
  • BibTeX: 44
  • EndNote: 41
Views and downloads (calculated since 27 Jun 2023)
Cumulative views and downloads (calculated since 27 Jun 2023)

Viewed (geographical distribution)

Total article views: 969 (including HTML, PDF, and XML) Thereof 921 with geography defined and 48 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 25 Jun 2024
Download
Short summary
Brinicles are tubular ice structures that grow under the sea ice in cold regions. This happens because the salty water going downwards from the sea ice is colder than the seawater. We have successfully recreated an analogue of these structures in our laboratory. Three methods were used, producing different results. In this paper, we explain how to use these methods and study the behaviour of the brinicles created when changing the flow of water and study the importance for natural brinicles.