Monitoring Seasonal Fluctuation and Long‐Term Trends for the Greenland Ice Sheet Using Seismic Noise Auto‐Correlations

Abstract One important feature of the Greenland Ice Sheet (GrIS) change is its strong seasonal fluctuation. Taking advantage of deployed seismographic stations in Greenland, we apply cross‐component auto‐correlation of seismic ambient noise to measure in‐situ near surface relative velocity change (d...

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Main Authors: Bingxu Luo, Shuo Zhang, Hejun Zhu
Format: Article
Language:English
Published: Wiley 2023-04-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1029/2022GL102146
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author Bingxu Luo
Shuo Zhang
Hejun Zhu
author_facet Bingxu Luo
Shuo Zhang
Hejun Zhu
author_sort Bingxu Luo
collection DOAJ
description Abstract One important feature of the Greenland Ice Sheet (GrIS) change is its strong seasonal fluctuation. Taking advantage of deployed seismographic stations in Greenland, we apply cross‐component auto‐correlation of seismic ambient noise to measure in‐situ near surface relative velocity change (dv/v) in different regions of Greenland. Our results demonstrate that dv/v measurements for most stations have less than 3 months lag times in comparison to the surface mass change. These various lag times may provide us constraints for the thickness of the subglacial till layer over different regions in Greenland. Moreover, in southwest Greenland, we observe a change in the long‐term trend of dv/v for three stations, which might be consistent with the mass change rate (dM/dt) due to the “2012–2013 warm‐cold transition.” These observations suggest that seismic noise auto‐correlation technique may be used to monitor both seasonal and long‐term changes of the GrIS.
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spelling doaj-art-57ab3bc34c7f443e85f030b0f6c208db2025-08-20T03:12:52ZengWileyGeophysical Research Letters0094-82761944-80072023-04-01507n/an/a10.1029/2022GL102146Monitoring Seasonal Fluctuation and Long‐Term Trends for the Greenland Ice Sheet Using Seismic Noise Auto‐CorrelationsBingxu Luo0Shuo Zhang1Hejun Zhu2Department of Geosciences The University of Texas at Dallas Richardson TX USADepartment of Geosciences The University of Texas at Dallas Richardson TX USADepartment of Geosciences The University of Texas at Dallas Richardson TX USAAbstract One important feature of the Greenland Ice Sheet (GrIS) change is its strong seasonal fluctuation. Taking advantage of deployed seismographic stations in Greenland, we apply cross‐component auto‐correlation of seismic ambient noise to measure in‐situ near surface relative velocity change (dv/v) in different regions of Greenland. Our results demonstrate that dv/v measurements for most stations have less than 3 months lag times in comparison to the surface mass change. These various lag times may provide us constraints for the thickness of the subglacial till layer over different regions in Greenland. Moreover, in southwest Greenland, we observe a change in the long‐term trend of dv/v for three stations, which might be consistent with the mass change rate (dM/dt) due to the “2012–2013 warm‐cold transition.” These observations suggest that seismic noise auto‐correlation technique may be used to monitor both seasonal and long‐term changes of the GrIS.https://doi.org/10.1029/2022GL102146auto‐correlationrelative velocity changeGreenland Ice Sheet
spellingShingle Bingxu Luo
Shuo Zhang
Hejun Zhu
Monitoring Seasonal Fluctuation and Long‐Term Trends for the Greenland Ice Sheet Using Seismic Noise Auto‐Correlations
Geophysical Research Letters
auto‐correlation
relative velocity change
Greenland Ice Sheet
title Monitoring Seasonal Fluctuation and Long‐Term Trends for the Greenland Ice Sheet Using Seismic Noise Auto‐Correlations
title_full Monitoring Seasonal Fluctuation and Long‐Term Trends for the Greenland Ice Sheet Using Seismic Noise Auto‐Correlations
title_fullStr Monitoring Seasonal Fluctuation and Long‐Term Trends for the Greenland Ice Sheet Using Seismic Noise Auto‐Correlations
title_full_unstemmed Monitoring Seasonal Fluctuation and Long‐Term Trends for the Greenland Ice Sheet Using Seismic Noise Auto‐Correlations
title_short Monitoring Seasonal Fluctuation and Long‐Term Trends for the Greenland Ice Sheet Using Seismic Noise Auto‐Correlations
title_sort monitoring seasonal fluctuation and long term trends for the greenland ice sheet using seismic noise auto correlations
topic auto‐correlation
relative velocity change
Greenland Ice Sheet
url https://doi.org/10.1029/2022GL102146
work_keys_str_mv AT bingxuluo monitoringseasonalfluctuationandlongtermtrendsforthegreenlandicesheetusingseismicnoiseautocorrelations
AT shuozhang monitoringseasonalfluctuationandlongtermtrendsforthegreenlandicesheetusingseismicnoiseautocorrelations
AT hejunzhu monitoringseasonalfluctuationandlongtermtrendsforthegreenlandicesheetusingseismicnoiseautocorrelations