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. 2024 Jun 27;11:702. doi: 10.1038/s41597-024-03472-0

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© The Author(s) 2024

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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Fig. 12 — In-ice light intensity profiles at the LM site on two exemplary days measured with the lightharp (downward planar $\underset{~}{d} ↓$ , upward planar $\underset{~}{u} ↑$ ) and lightchain 2020R11 (sideward planar →). Shown are measurements with the three VIS color bands R, G, and B, scaled with the downwelling planar intensity at radiation station 2020R11¹². The grey box shows the vertical extent of the ice, and the blue box shows the extent of the snow layer retrieved from 2019T62²⁴.