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. 2022 Sep 2;11:261. doi: 10.1038/s41377-022-00951-0

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© The Author(s) 2022

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 license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license 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 license, visit http://creativecommons.org/licenses/by/4.0/.

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Fig. 4 — Plots of a water depth from ETOPO1, b Chl, c SSC, d a_CDOM from HY-1C (Methods) with the ship track in red lines. Profiles of e b_bp, f K_d, g R retrieved by HSRL with 3 optical depths in red lines. Discrete in situ data were collected at different time T₁-T₅ (Methods)