Abstract
Vertical circulation reaches the bottom of the deepest (> 90 m) part of the northern basin of Lake Biwa, a warm monomictic lake, during winter (January to March) every year. In winter 2019, we found non-circulated water masses at the bottom of the lake where the basin is 90 m deep. This is the first observation of an incomplete vertical circulation event since we started monitoring Lake Biwa in 1979. Analysis of water quality monitoring and meteorological data shows that weaker cooling and weaker winds during winter 2019 affected vertical circulation. Dissolved oxygen concentrations in the bottom layer recovered even after the appearance of a seasonal thermocline. However, the concentrations remained below that in the surface layer.
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Acknowledgements
We thank Professor Shin-ichi Nakano of Kyoto University for his valuable comments and suggestions. The first author of this paper, Mr. Kenta Yamada passed away in November 2020 after submission. He was a researcher at Lake Biwa Environmental Research Institute, and had a passion for monitoring and researching the water environment in Lake Biwa. He remains in our memory for his lake monitoring and research work and also for compiling this paper and making significant contributions to it.
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Yamada, K., Yamamoto, H., Hichiri, S. et al. First observation of incomplete vertical circulation in Lake Biwa. Limnology 22, 179–185 (2021). https://doi.org/10.1007/s10201-021-00653-3
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DOI: https://doi.org/10.1007/s10201-021-00653-3