EGU26-14408, updated on 14 Mar 2026
https://doi.org/10.5194/egusphere-egu26-14408
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
PICO | Monday, 04 May, 16:17–16:19 (CEST)
 
PICO spot 1a, PICO1a.2
Feeling the heat: global detection of volcanic effects on glacier mass balance and dynamics
Tryggvi Unnsteinsson1, Matteo Spagnolo2, Brice Rea1, Társilo Girona3, Iestyn Barr4, and Donal Mullan5
Tryggvi Unnsteinsson et al.
  • 1University of Aberdeen, Department of Geography and Environment, Aberdeen, UK (t.unnsteinsson.23@abdn.ac.uk)
  • 2Department of Earth Sciences, University of Torino, Torino, Italy
  • 3Geosciences Barcelona (GEO3BCN-CSIC), Barcelona, Spain
  • 4Department of Natural Sciences, Manchester Metropolitan University, Manchester, UK
  • 5School of Natural and Built Environment, Queen’s University Belfast, Belfast, NI, UK

With the availability of open-access satellite imagery and derived products from open-source tools, global studies of glaciers have become increasingly manageable. Many studies have used these global datasets to delineate spatial and temporal variations in glacier mass balance and dynamics. This has highlighted the effects of seasonal fluctuations and climatic trends on glaciers and has aided the identification of glacier surges. Here we focus on the often-neglected effects volcanoes may have on glacier mass balance and dynamics. First, we analyse the elevation distribution of the world’s glaciers with respect to their proximity to volcanoes and find that there is measurable evidence of the negative mass-balance effect volcanoes have on nearby glaciers. Second, we use the ITS_LIVE glacier velocity dataset along with the new TICOI regularisation and signal decomposition to identify velocity anomalies on glaciers located around volcanoes. This allows us to discern both short-lived velocity anomalies as well as long-term trends and variations in seasonal patterns. We identify multiple velocity anomalies, many of which correlate with climatic trends or weather events, others with surges, but some stand out as volcanically induced. We demonstrate examples of what effect various volcanic processes such as geothermal activity, mass wasting events, unrest, and pre-eruptive activity can have on glacier velocity.

How to cite: Unnsteinsson, T., Spagnolo, M., Rea, B., Girona, T., Barr, I., and Mullan, D.: Feeling the heat: global detection of volcanic effects on glacier mass balance and dynamics, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-14408, https://doi.org/10.5194/egusphere-egu26-14408, 2026.