Award Abstract # 2025563
Using machine learning method to detect slow slip events in ocean bottom pressure data

NSF Org: OCE
Division Of Ocean Sciences
Recipient: UNIVERSITY OF RHODE ISLAND
Initial Amendment Date: July 1, 2020
Latest Amendment Date: May 4, 2022
Award Number: 2025563
Award Instrument: Standard Grant
Program Manager: Scott M. White
scwhite@nsf.gov
 (703)292-8369
OCE
 Division Of Ocean Sciences
GEO
 Directorate for Geosciences
Start Date: July 1, 2020
End Date: June 30, 2025 (Estimated)
Total Intended Award Amount: $406,376.00
Total Awarded Amount to Date: $446,376.00
Funds Obligated to Date: FY 2020 = $406,376.00
FY 2022 = $40,000.00
History of Investigator:
  • Meng Wei (Principal Investigator)
    matt-wei@uri.edu
  • Yang Shen (Co-Principal Investigator)
  • Marco Alvarez (Co-Principal Investigator)
Recipient Sponsored Research Office: University of Rhode Island
75 LOWER COLLEGE RD RM 103
KINGSTON
RI  US  02881-1974
(401)874-2635
Sponsor Congressional District: 02
Primary Place of Performance: University of Rhode Island
215 S Ferry Rd
Narragansett
RI  US  02882-1197
Primary Place of Performance
Congressional District:
02
Unique Entity Identifier (UEI): CJDNG9D14MW7
Parent UEI: NSA8T7PLC9K3
NSF Program(s): PHYSICAL OCEANOGRAPHY,
Marine Geology and Geophysics
Primary Program Source: 01002223DB NSF RESEARCH & RELATED ACTIVIT
01002021DB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s): 1610, 1620
Program Element Code(s): 161000, 162000
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

This project seeks to improve the understanding of earthquakes and tsunamis in subduction zones. Special tectonic signals that can be measured at the seafloor may represent the release of tectonic stress in subduction zones. If so, measurements from pressure sensors on the seafloor could be used to estimate earthquake and tsunami risks. However, noise from ocean processes makes it difficult to detect this signal accurately. This project will take advantage of recent advances in a computational technique, machine learning, to develop a better detector of this signal.. This project will support early career scientists and people from underrepresented groups (Latino and Female) in STEM fields. It will also support a graduate student and several undergraduates. This project will develop teaching modules of machine learning at the graduate, undergraduate, high school, and middle school levels. This project will publish code in the public domain and share the teaching modules within the community immediately after the project finishes.

Shallow slow slip events provide a mechanism for strain release at the shallow part of subduction zones, which is important for tsunami hazard assessment. For most subduction zones, the trench is far from the coast and it is unclear whether shallow slow slip events exist. Even in places where these events were detected, key quantities such as the duration and magnitude were not well constrained. As a result, the locking state of shallow subduction zones and the mechanism of shallow slow slip events is still unclear. To answer these questions, this project will take advantage of recent advancement in machine learning and the accumulation of seafloor pressure datasets to improve our ability to detect shallow slow slip events in subduction zones. Preliminary analyses of seafloor pressure data from New Zealand have demonstrated that machine learning can successfully identify known slow slip events and further reduce ocean noise in seafloor pressure data. Using available data from several subduction zones, this project will further improve the machine-learning detector to estimate the duration, amplitude, and timing of shallow slow slip events. This project will also develop an improved way to reduce ocean noise in seafloor pressure data by using machine learning to capture the complex relationship of measurable quantities in the ocean. Collectively, this project will provide better tools to measure shallow slow slip events and assess the locking state of shallow subduction zones.

This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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He, Bing and Wei, XiaoZhuo and Wei, Meng and Shen, Yang and Alvarez, Marco and Schwartz, Susan Y. "A shallow slow slip event in 2018 in the Semidi segment of the Alaska subduction zone detected by machine learning" Earth and Planetary Science Letters , v.612 , 2023 https://doi.org/10.1016/j.epsl.2023.118154 Citation Details

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