Articles | Volume 12, issue 1
https://doi.org/10.5194/essd-12-231-2020
https://doi.org/10.5194/essd-12-231-2020
Data description paper
 | 
05 Feb 2020
Data description paper |  | 05 Feb 2020

Paleo-hydrologic reconstruction of 400 years of past flows at a weekly time step for major rivers of Western Canada

Andrew R. Slaughter and Saman Razavi

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Cited articles

Agafonov, L. I., Meko, D. M., and Panyushkina, I. P.: Reconstruction of Ob River, Russia, discharge from ring widths of floodplain trees, J. Hydrol., 543, 198–207, 2016. 
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Axelson, J. N., Sauchyn, D. J., and Barichivich, J.: New reconstructions of streamflow variability in the South Saskatchewan River Basin from a network of tree ring chronologies, Alberta, Canada, Water Resour. Res., 45, W09422, https://doi.org/10.1029/2008WR007639, 2009. 
Boucher, Ė., Ouarda, T. B. M. J., Bėgin, Y., and Nicault, A.: Spring flood reconstruction from continuous and discrete tree ring series, Water Resour. Res., 47, W07516, https://doi.org/10.1029/2010WR010131, 2011. 
Brigode, P., Brissette, F., Nicault, A., Perreault, L., Kuentz, A., Mathevet, T., and Gailhard, J.: Streamflow variability over the 1881–2011 period in northern Québec: comparison of hydrological reconstructions based on tree rings and geopotential height field reanalysis, Clim. Past, 12, 1785–1804, https://doi.org/10.5194/cp-12-1785-2016, 2016. 
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Short summary
Water management faces the challenge of non-stationarity in future flows. To extend flow datasets beyond the gauging data, this study presents a method of generating an ensemble of weekly flows from tree-ring reconstructed flows to represent uncertainty that can overcome certain long-standing data challenges with paleo-reconstruction. An ensemble of 500 flow time series were generated for the four sub-basins of the Saskatchewan River basin, Canada, for the period 1600–2001.
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