- 1University of Genoa, DIBRIS, Genova, Italy (giulia.blandini@cimafoundation.org)
- 2CIMA Research Foundation, Savona,Italy
- 3Department of Geosciences, University of Oslo, Oslo, Norway
- 4Department of Environmental Science, Policy, and Management, University of California, Berkeley, Berkeley, CA, United States of America
- 5Snow and Ice Research Center, National Research Institute for Earth Science and Disaster Resilience, Nagaoka, Japan
In snow-dominated regions, today’s snow is tomorrow’s water, making reliable estimates of snow water equivalent (SWE) and snow depth crucial for water resource management. In this context, data assimilation is a powerful tool to optimally combine models and measurements, enhancing accuracy and reliability. Ensemble-based techniques like the Ensemble Kalman Filter (EnKF) and Particle Filter (PF) are often used but their deployment in real-time applications can make it challenging to ensure timely and accurate results. To address these challenges, we propose an innovative data assimilation framework for snow hydrology that leverages Long Short-Term Memory (LSTM) networks. Using data from seven diverse study sites across the Northern Hemisphere, our framework is trained on the outputs of an EnKF, persuing a balance between computational efficiency and model complexity to advance data assimilation applications in snow hydrology. This LSTM-based framework achieves performance comparable to the EnKF in improving open-loop estimates, with only minor increases in root-mean-square error (RMSE): +6 mm for SWE and +6 cm for snow depth on average. Adding a memory component enhances stability and accuracy, especially under sparse data conditions. When trained on long-term datasets spanning 25 years, the LSTM framework demonstrated promising spatial transferability, with accuracy reductions of less than 20% for snow water equivalent and snow depth estimation. After training, the LSTM approach significantly outperformed a parallelized EnKF in computational efficiency, reducing runtime by 70% while maintaining comparable accuracy. Training on multi-site data further ensured robust performance across diverse climate regimes and during both dry and average water years, with a modest RMSE increase compared to the EnKF (+6 mm for SWE and +18 cm for snow depth). By combining the strengths of traditional ensemble methods and modern machine learning, this framework offers a scalable, computationally efficient, and reliable alternative for operational snow hydrology data assimilation.
How to cite: Blandini, G., Avanzi, F., Campo, L., Gabellani, S., Aalstad, K., Girotto, M., Yamaguchi, S., Hirashima, H., and Ferraris, L.: Learning to filter: Snow data assimilation using a Long Short-Term Memory network, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-17427, https://doi.org/10.5194/egusphere-egu25-17427, 2025.