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. 2019 Jul 1;9:9442. doi: 10.1038/s41598-019-45077-3

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© The Author(s) 2019

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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Water masses in Kongsfjorden during 2013, 2014, and 2016. Panels A and B (2013 and 2014) are adapted from the results reported by Prominska et al.²³. Panel C shows the locations of the SVP profiles taken during the course of this study (green dots) during August 2016. Panel D is a conceptual sketch of the water masses present in the inner fjord, based on a number of profiles (shown in bold) taken at the locations shown in panel C. Note the different depth and longitude scales in panel D compared by panels A and B. In the legend, Atlantic water is denoted AW, Transformed Atlantic water is TAW, Intermediate water is IW, Surface water is SW, and Local water is LW. More detail on these classifications in available in the methods. The background image in panel C is Copernicus Sentinel data (2016) downloaded from the Copernicus Open Access Hub (https://scihub.copernicus.eu/). Terms of use available at https://scihub.copernicus.eu/twiki/do/view/SciHubWebPortal/TermsConditions. Panels A, B, and D were created in R³⁶.