Predicting glacial runoff in a changing climate

How HydroForecast builds resilience in glacial environments
Melanie Feen
Aug 18, 2025
Table of contents

Hydropower is a crucial source of renewable energy, but its efficiency can be significantly impacted by the water availability. Glaciers pose unique challenges to forecasting water availability due to their dynamic nature and fluctuating meltwater contributions. HydroForecast offers a powerful solution to optimize hydropower operations in complex glacial environments.

"Matanuska Glacier from parking lot." May 20, 2008, by Frank K. licensed under CC BY 2.0

The challenges of managing hydropower in glaciated areas

Glacier-fed river basins play an important role in global hydropower, but they also bring unique challenges for energy generation. Recent studies estimate that, around the world, there are roughly 185,000 glacierized sites contributing 13% of global hydropower. In Norway, glacier melt drives about 15% of the nation’s hydroelectric output. Given that glaciers hold roughly 69% of Earth’s freshwater, their influence on hydropower operations and planning is substantial, both now and in the face of a changing climate.

  • Climate change: Changes in historical weather patterns are leading to accelerated glacial melt, altering the timing and volume of runoff, and impacting the once reliable volume of baseflow derived from glaciers. This has significant, yet understudied implications for long-term hydropower resource planning  in glaciated basins. 
  • Modeling limitations: Popular physical models are not designed to predict glacial hydrology. Glacial melt is influenced primarily by temperature, snowfall, and albedo. Standard hydrologic models lack inherent representation of these processes and require additional modules to predict glacier contributions to streamflow. While data-driven approaches are showing promise in capturing these dynamics, they are not yet widely integrated.
  • Lack of reliable data: Traditional forecasting methods require site-specific calibration using historical water data, but remote glacier regions often lack this data, making these methods unreliable. Additionally, ice and cold weather can impact streamflow gauges leading to data outages during critical periods.

How HydroForecast powers hydropower in glaciated basins

HydroForecast combines an advanced machine learning hydrologic model with weather forecasts and satellite imagery inputs to address these modeling challenges.

A blended approach: Machine learning meets data

HydroForecast is trained on time series of satellite imagery, weather, and streamflow data and optimized to make the best prediction of total streamflow at each time step. These inputs enable the model to identify complex relationships and patterns that occur in glaciated basins, thus simplifying the solution into a single accurate model.

Adaptive management for long-term planning

As glacial dynamics shift due to climate change, HydroForecast continuously learns and adapts to real-time basin conditions. For example, the model  tracks the evolution of snowpack and snow cover through satellite data. As hydropower maintains a critical role in the energy mix, HydroForecast’s ability to predict melt and big changes in glacial systems is key for ensuring long-term supply.

Designed to capture cold weather dynamics

To continuously improve our model's accuracy in glaciated regions, we trained HydroForecast on over 2,000 gauges in Canada to better learn cold-weather hydrology.

Real-world examples of HydroForecast in glacial catchments

Throughout the day, hourly streamflow varies due to temperature fluctuations.

Below are examples of the HydroForecast dashboard before and after tuning the model to better capture these streamflow fluctuations due to glaciers. Prior to tuning, the model had already learned the basics of diurnal fluctuation, recognizing this pattern in snowmelt regions at large. Now, when operationalizing HydroForecast in glaciated basins, we add special parameters to handle the sensitivity of glaciers.

In addition to diurnal cycles, the majority of baseflow during the summer months in these regions is due to glacial melt. In the example below, the mean line accurately captures the magnitude of flow and the timing of the diurnal cycles 10-days ahead — with the added complexity of rain in the forecast.

Curious to learn how HydroForecast can work in your glaciated region? Reach out to our team to learn more.

Updated Button Contact us