Long-Term Infrasonic Monitoring of Land and Marine-Terminating Glaciers in Greenland

Journal Article (2022)
Authors

Laslo Evers (Royal Netherlands Meteorological Institute (KNMI), TU Delft - Applied Geophysics and Petrophysics)

Pieter S.M. Smets (TU Delft - Applied Geophysics and Petrophysics)

J. D. Assink (Royal Netherlands Meteorological Institute (KNMI))

S. Shani-Kadmiel (Royal Netherlands Meteorological Institute (KNMI))

K Kondo (Hokkaido University)

S. Sugiyama (Hokkaido University)

Research Group
Applied Geophysics and Petrophysics
Copyright
© 2022 L.G. Evers, P.S.M. Smets, J. D. Assink, Shahar Shani-Kadmiel, K. Kondo, S. Sugiyama
To reference this document use:
https://doi.org/10.1029/2021GL097113
More Info
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Publication Year
2022
Language
English
Copyright
© 2022 L.G. Evers, P.S.M. Smets, J. D. Assink, Shahar Shani-Kadmiel, K. Kondo, S. Sugiyama
Research Group
Applied Geophysics and Petrophysics
Issue number
8
Volume number
49
Pages (from-to)
1-8
DOI:
https://doi.org/10.1029/2021GL097113
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Abstract

A period of 18 years of infrasonic recordings was analyzed from a microbarometer array (I18DK) in northwestern Greenland, near Qaanaaq. A huge number of infrasonic detections, over 700,000, have been made in I18DKs soundscape during the Arctic summers. Simultaneously identified were both calving events from marine-terminating glaciers and discharge related acoustics from a land-terminating glacier. This infrasonic activity is correlated to sea-surface and atmospheric temperature, respectively. Inter-yearly to daily variations were retrieved showing a strong variability in infrasonic detection rates and hence glacier activity. The highest number of infrasonic detections were found in recent years from the land-terminating glacier. The latter is supported by actual discharge measurements and partly by a discharge model. It is concluded that monitoring infrasound from glaciers can complement other techniques to remotely and passively get insights into glacier dynamics with high temporal and spatial resolution.