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Title: Insights into Permafrost and Seasonal Active-Layer Dynamics from Ambient Seismic Noise Monitoring

Journal Article · · Journal of Geophysical Research. Earth Surface
DOI:https://doi.org/10.1029/2019JF005051· OSTI ID:1528869
ORCiD logo [1];  [2]; ORCiD logo [2]; ORCiD logo [3]; ORCiD logo [4]
  1. Univ. of Florida, Gainesville, FL (United States); U.S. Geological Survey, Denver, CO (United States)
  2. Sandia National Lab. (SNL-NM), Albuquerque, NM (United States)
  3. California Inst. of Technology (CalTech), Pasadena, CA (United States)
  4. Univ. of Florida, Gainesville, FL (United States)
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Abstract Widespread permafrost thaw in response to changing climate conditions has the potential to dramatically impact ecosystems, infrastructure, and the global carbon budget. Ambient seismic noise techniques allow passive subsurface monitoring that could provide new insights into permafrost vulnerability and active‐layer processes. Using nearly 2 years of continuous seismic data recorded near Fairbanks, Alaska, we measured relative velocity variations that showed a clear seasonal cycle reflecting active‐layer freeze and thaw. Relative to January 2014, velocities increased up to 3% through late spring, decreased to −8% by late August, and then gradually returned to the initial values by the following winter. Velocities responded rapidly (over ~2 to 7 days) to discrete hydrologic events and temperature forcing and indicated that spring snowmelt and infiltration events from summer rainfall were particularly influential in propagating thaw across the site. Velocity increases during the fall zero‐curtain captured the refreezing process and incremental ice formation. Looking across multiple frequency bands (3–30 Hz), negative relative velocities began at higher frequencies earlier in the summer and then shifted lower when active‐layer thaw deepened, suggesting a potential relationship between frequency and thaw depth; however, this response was dependent on interstation distance. Bayesian tomography returned 2‐D time‐lapse images identifying zones of greatest velocity reduction concentrated in the western side of the array, providing insight into the spatial variability of thaw progression, soil moisture, and drainage. This study demonstrates the potential of passive seismic monitoring as a new tool for studying site‐scale active‐layer and permafrost thaw processes at high temporal and spatial resolution.

Research Organization:
Sandia National Lab. (SNL-NM), Albuquerque, NM (United States)
Sponsoring Organization:
USDOE National Nuclear Security Administration (NNSA)
Grant/Contract Number:
AC04-94AL85000; DE‐NA0003525
OSTI ID:
1528869
Alternate ID(s):
OSTI ID: 1542506
Report Number(s):
SAND-2019-6690J; SAND-2019-2136J; 676448
Journal Information:
Journal of Geophysical Research. Earth Surface, Vol. 124, Issue 7; ISSN 2169-9003
Publisher:
American Geophysical UnionCopyright Statement
Country of Publication:
United States
Language:
English
Citation Metrics:
Cited by: 35 works
Citation information provided by
Web of Science

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Cited By (2)

Seismic Noise in Central Alaska and Influences From Rivers, Wind, and Sedimentary Basins journal November 2019
Joint Sensing of Bedload Flux and Water Depth by Seismic Data Inversion journal November 2019

Figures / Tables (8)

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Related Subjects

58 GEOSCIENCES
ambient seismic noise
permafrost
active layer
velocity variations
seismic interferometry