Articles | Volume 18, issue 8
https://doi.org/10.5194/essd-18-6101-2026
https://doi.org/10.5194/essd-18-6101-2026
Data description article
 | 
26 Aug 2026
Data description article |  | 26 Aug 2026

A 225-year (1799–2024) homogenized daily water level series of the Vistula River in Warsaw

Łukasz Sobechowicz, Dariusz Brykała, Ewa Kaznowska, Michał Wasilewicz, Jacek Wolski, Marcin Noras, and Wojciech Aleksander Siwek

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Cited articles

Biernacki, Z.: Geomorphology and Surface Waters, in: The Vistula in Warsaw, edited by: J. Lickiewicz, J. Pawlak, and W. Pietrusiewicz, Office of the Capital City of Warsaw, Department of Spatial Planning and Architecture, Warsaw, 22–70, https://architektura.um.warszawa.pl/documents/12025039/26157681/Wisla_w_Warszawie_0.pdf/b1db8df9-e04e-4f10-9f0f-44ac20901c6d?t=1634497946935 (last access: 21 August 2026), 2000 (in Polish). 
Bogdanowicz, E., Fal, B., and Dobrzyńska, I.: Hydrological Characteristics, in: The Vistula in Warsaw, edited by J. Lickiewicz, J. Pawlak, and W. Pietrusiewicz, Office of the Capital City of Warsaw, Department of Spatial Planning and Architecture, Warsaw, 9–13, https://architektura.um.warszawa.pl/documents/12025039/26157681/Wisla_w_Warszawie_0.pdf/b1db8df9-e04e-4f10-9f0f-44ac20901c6d?t=1634497946935 (last access: 21 August 2026), 2000 (in Polish). 
Brázdil, R., Kundzewicz, Z. W., and Benito G.: Historical hydrology for studying flood risk in Europe, Hydrological Sciences–Journal–des Sciences Hydrologiques, 51, 739–764, https://doi.org/10.1623/hysj.51.5.739, 2006. 
Brönnimann, S., Frigerio, L., Schwander, M., Rohrer, M., Stucki, P., and Franke, J.: Causes of increased flood frequency in central Europe in the 19th century, Clim. Past, 15, 1395–1409, https://doi.org/10.5194/cp-15-1395-2019, 2019. 
Byczkowski, A.: Hydrology, Vol. I, Wydawnictwo SGGW, Warsaw, 375 pp., ISBN 83-00-02925-7, 1996 (in Polish). 
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We present a 225-year (1799–2024) homogenized daily water level record for the Vistula River in Warsaw, comprising 82 453 observations. Adjustments were made for gauge relocations, zero shifts, unit differences, and Julian–Gregorian discrepancies. Missing data were reconstructed using the Long Short-Term Memory (LSTM) method, applied to stage–stage relationships with downstream stations. The dataset provides a robust basis for long-term hydrological, climatic, and socio-environmental research.
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