Monitoring Terrestrial Water Storage, Drought and Seasonal Changes in Central Oklahoma With Ambient Seismic Noise

Abstract Significant imbalances in terrestrial water storage (TWS) and severe drought have been observed around the world as a consequence of climate changes. Improving our ability to monitor TWS and drought is critical for water‐resource management and water‐deficit estimation. We use continuous se...

Full description

Saved in:
Bibliographic Details
Main Authors: Shuo Zhang, Bingxu Luo, Yehuda Ben‐Zion, David E. Lumley, Hejun Zhu
Format: Article
Language:English
Published: Wiley 2023-09-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1029/2023GL103419
Tags: Add Tag
No Tags, Be the first to tag this record!
_version_ 1849761289058910208
author Shuo Zhang
Bingxu Luo
Yehuda Ben‐Zion
David E. Lumley
Hejun Zhu
author_facet Shuo Zhang
Bingxu Luo
Yehuda Ben‐Zion
David E. Lumley
Hejun Zhu
author_sort Shuo Zhang
collection DOAJ
description Abstract Significant imbalances in terrestrial water storage (TWS) and severe drought have been observed around the world as a consequence of climate changes. Improving our ability to monitor TWS and drought is critical for water‐resource management and water‐deficit estimation. We use continuous seismic ambient noise to monitor temporal evolution of near‐surface seismic velocity, dv/v, in central Oklahoma from 2013 to 2022. The derived dv/v is found to be negatively correlated with gravitational measurements and groundwater depths, showing the impact of groundwater storage on seismic velocities. The hydrological effects involving droughts and recharge of groundwater occur on a multi‐year time scale and dominate the overall derived velocity changes. The thermoelastic response to atmospheric temperature variations occurs primarily on a yearly timescale and dominates the superposed seasonal velocity changes in this study. The occurrences of droughts appear simultaneously with local peaks of dv/v, demonstrating the sensitivity of near‐surface seismic velocities to droughts.
format Article
id doaj-art-de00aa4d0ba74c7a9ceb8a1a99fb99c9
institution DOAJ
issn 0094-8276
1944-8007
language English
publishDate 2023-09-01
publisher Wiley
record_format Article
series Geophysical Research Letters
spelling doaj-art-de00aa4d0ba74c7a9ceb8a1a99fb99c92025-08-20T03:06:04ZengWileyGeophysical Research Letters0094-82761944-80072023-09-015017n/an/a10.1029/2023GL103419Monitoring Terrestrial Water Storage, Drought and Seasonal Changes in Central Oklahoma With Ambient Seismic NoiseShuo Zhang0Bingxu Luo1Yehuda Ben‐Zion2David E. Lumley3Hejun Zhu4Department of Geosciences The University of Texas at Dallas Richardson TX USADepartment of Geosciences The University of Texas at Dallas Richardson TX USADepartment of Earth Science and Southern California Earthquake Center University of Southern California Los Angeles CA USADepartment of Geosciences The University of Texas at Dallas Richardson TX USADepartment of Geosciences The University of Texas at Dallas Richardson TX USAAbstract Significant imbalances in terrestrial water storage (TWS) and severe drought have been observed around the world as a consequence of climate changes. Improving our ability to monitor TWS and drought is critical for water‐resource management and water‐deficit estimation. We use continuous seismic ambient noise to monitor temporal evolution of near‐surface seismic velocity, dv/v, in central Oklahoma from 2013 to 2022. The derived dv/v is found to be negatively correlated with gravitational measurements and groundwater depths, showing the impact of groundwater storage on seismic velocities. The hydrological effects involving droughts and recharge of groundwater occur on a multi‐year time scale and dominate the overall derived velocity changes. The thermoelastic response to atmospheric temperature variations occurs primarily on a yearly timescale and dominates the superposed seasonal velocity changes in this study. The occurrences of droughts appear simultaneously with local peaks of dv/v, demonstrating the sensitivity of near‐surface seismic velocities to droughts.https://doi.org/10.1029/2023GL103419Oklahomaambient seismic noisegroundwater monitoringvelocity variationsthermo‐elastic strain
spellingShingle Shuo Zhang
Bingxu Luo
Yehuda Ben‐Zion
David E. Lumley
Hejun Zhu
Monitoring Terrestrial Water Storage, Drought and Seasonal Changes in Central Oklahoma With Ambient Seismic Noise
Geophysical Research Letters
Oklahoma
ambient seismic noise
groundwater monitoring
velocity variations
thermo‐elastic strain
title Monitoring Terrestrial Water Storage, Drought and Seasonal Changes in Central Oklahoma With Ambient Seismic Noise
title_full Monitoring Terrestrial Water Storage, Drought and Seasonal Changes in Central Oklahoma With Ambient Seismic Noise
title_fullStr Monitoring Terrestrial Water Storage, Drought and Seasonal Changes in Central Oklahoma With Ambient Seismic Noise
title_full_unstemmed Monitoring Terrestrial Water Storage, Drought and Seasonal Changes in Central Oklahoma With Ambient Seismic Noise
title_short Monitoring Terrestrial Water Storage, Drought and Seasonal Changes in Central Oklahoma With Ambient Seismic Noise
title_sort monitoring terrestrial water storage drought and seasonal changes in central oklahoma with ambient seismic noise
topic Oklahoma
ambient seismic noise
groundwater monitoring
velocity variations
thermo‐elastic strain
url https://doi.org/10.1029/2023GL103419
work_keys_str_mv AT shuozhang monitoringterrestrialwaterstoragedroughtandseasonalchangesincentraloklahomawithambientseismicnoise
AT bingxuluo monitoringterrestrialwaterstoragedroughtandseasonalchangesincentraloklahomawithambientseismicnoise
AT yehudabenzion monitoringterrestrialwaterstoragedroughtandseasonalchangesincentraloklahomawithambientseismicnoise
AT davidelumley monitoringterrestrialwaterstoragedroughtandseasonalchangesincentraloklahomawithambientseismicnoise
AT hejunzhu monitoringterrestrialwaterstoragedroughtandseasonalchangesincentraloklahomawithambientseismicnoise