Acoustic signals provide alternative method of monitoring glacial runoff

Acoustic signals used to monitor glacial runoff could provide a cheaper and more accessible alternative to existing methods such as fibre-optic tools.

Traditional methods of estimating glacier discharge involve water depth measurements, a physically demanding task that requires wading into the fast flowing, freezing cold water
Traditional methods of estimating glacier discharge involve water depth measurements, a physically demanding task that requires wading into the fast flowing, freezing cold water - Shin Sugiyama

Scientists monitor melting glaciers to gauge the meltwater contribution to ocean and freshwater resources globally, while also observing the risk of glacial flooding. However, glacio-hydrological monitoring is expensive, requiring a substantial effort by observers or sophisticated technology with large volumes of data.

Now, scientists from Japan’s Hokkaido University, led by Evgeny A. Podolskiy, have proposed a safe, affordable, and effective approach for monitoring glacial discharge using sounds generated at the proglacial run-off site. The method, published in Geophysical Research Letters, is reportedly approximately 100 times cheaper than the most novel methods, non-invasive, quick to deploy, and can become a tool for long-term glacier monitoring.

Previous research linked inaudible (infrasound) signals to glacial runoffs, noting a daily variation in the recordings and a peak during the summer. It was hypothesised that these signals might be generated by the radiation of air-pressure waves from the glacial runoff. Consequently, it was suggested that glacier discharge could be measured by analysing the audible sounds that are also emitted by melting glaciers.

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