EGU24-13915, updated on 09 Mar 2024
https://doi.org/10.5194/egusphere-egu24-13915
EGU General Assembly 2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

FROSTBYTE: A reproducible data-driven workflow for probabilistic seasonal streamflow forecasting in snow-fed river basins across North America

Louise Arnal1,2, Martyn P. Clark1,3, Alain Pietroniro3, Vincent Vionnet4, David R. Casson3, Paul H. Whitfield1, Vincent Fortin4, Andrew W. Wood5,6, Wouter J. M. Knoben3, Brandi W. Newton7, and Colleen Walford8
Louise Arnal et al.
  • 1Centre for Hydrology, Coldwater Laboratory, University of Saskatchewan, Canmore, AB, Canada
  • 2Climate Scenarios and Services Team, Ouranos, Montreal, Canada
  • 3Department of Civil Engineering, University of Calgary, Calgary, AB, Canada
  • 4Meteorological Research Division, Environment and Climate Change Canada, Dorval, QC, Canada
  • 5National Center for Atmospheric Research, Boulder, CO, USA
  • 6Colorado School of Mines, Golden, CO, USA
  • 7Airshed and Watershed Stewardship Branch, Alberta Environment and Protected Areas, Calgary, AB, Canada
  • 8Alberta River Forecast Center, Environment and Protected Areas, Government of Alberta, Edmonton, AB, Canada

Seasonal streamflow forecasts provide key information for decision-making in sectors such as water supply management, hydropower generation, and irrigation scheduling. Principal component regression (PCR) stands as a well-established and widely used data-driven method for seasonal streamflow forecasting, offering advantages over more complex methods, including intuitive use of local data to represent key hydrological processes and low computational resource requirements.

We will present FROSTBYTE, a systematic and reproducible data-driven workflow for probabilistic seasonal streamflow forecasting in snow-fed river basins. FROSTBYTE is available on GitHub as a collection of Jupyter Notebooks, facilitating broader applications in cold regions and contributing to the ongoing advancement of methodologies. This structured workflow consists of five essential steps: 1) Regime classification and basins selection, 2) Streamflow pre-processing, 3) Snow Water Equivalent (SWE) pre-processing, 4) Forecasting using PCR, and 5) Hindcast verification. It was applied to 75 basins characterized by a snowmelt-driven regime and limited regulation across diverse North American geographies and climates. Ensemble hindcasts of winter to summer streamflow volumes were generated from 1979 to 2021, with initialization dates ranging from January 1st to September 1st. The hindcasts were evaluated with a user-oriented approach, tailored to offer insights for snow monitoring experts, forecasters, decision-makers, and workflow developers. Join us to learn more about FROSBYTE, and explore ways in which you can actively contribute to its development.

How to cite: Arnal, L., Clark, M. P., Pietroniro, A., Vionnet, V., Casson, D. R., Whitfield, P. H., Fortin, V., Wood, A. W., Knoben, W. J. M., Newton, B. W., and Walford, C.: FROSTBYTE: A reproducible data-driven workflow for probabilistic seasonal streamflow forecasting in snow-fed river basins across North America, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-13915, https://doi.org/10.5194/egusphere-egu24-13915, 2024.