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. 2023 Mar 29;13:5132. doi: 10.1038/s41598-023-31640-6

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© The Author(s) 2023

Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/.

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Evaporation flux distribution in stage 2. (a) Schematic of evaporation flux distribution at crust top surface and absorption flux distribution at crust bottom surface during the salt crust destabilization period; vertical pixel lines considered in the image processing (see the “Materials and Methods “section). It can be noted that the distance $h_{t}$ can be locally equal to zero since some fingers reach the cell top. The average distance over the vertical lines shown in the figure is however greater than zero, (b) salt crust top surface displacement along lines 3, 11 and 13 (selected because corresponding to finger tips). The inset shows the crust top surface mean displacement as a function of the evaporation rate (up to day 1.5).