Ettore Biondi
Assistant Professor of Geophysics
Bio
My research centers on leveraging fiber sensing technologies and dense seismic sensor networks for geophysical applications. By capturing vibrations from human activities and natural events such as ocean waves and earthquakes, my group develops methods to interpret the underlying mechanisms and subsurface structures driving these processes, including volcanic system dynamics and earthquake physics. With the rise of fiber sensing, we are exploring innovative approaches to create new environmental sensors that track both short- and long-term climate-related changes. I am also interested in using specialized sensor deployments in remote areas, such as glaciers and large volcanic systems, to investigate complex geophysical mechanisms. Additionally, our research aims to design advanced early warning systems for volcanoes, earthquakes, and tsunamis using long-term seismic arrays based on telecommunications fibers.
Boards, Advisory Committees, Professional Organizations
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Advisor and Board Member, Vortex Imaging (2024 - Present)
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Advisor, Google X (2024 - Present)
Professional Education
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PhD, Stanford University, Geophysics (2021)
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Diploma, Scuola Normale Superiore of Pisa, Computational Chemistry (2013)
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MSc, University of Pisa, Geophysics (2012)
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BSc, University of Genoa, Geology (2010)
Patents
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Jiaxuan Li, Ettore Biondi, Weiqiang Zhu, Zhongwen Zhan. "United States Patent 18/770,303 Inverting earthquake focal mechanisms with distributed acoustic sensing", California Institute of Technology, Jan 16, 2025
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Ettore Biondi, Jiaxuan Li, Weiqiang Zhu, Zhongwen Zhan. "United States Patent 18/752,231 Fiber-seismic tomography", California Institute of Technology, Dec 26, 2024
Current Research and Scholarly Interests
Ettore Biondi's research focuses on advancing distributed fiber-optic sensing technologies for the study of Earth system phenomena. His interdisciplinary work bridges geophysics, environmental engineering, and data science, exploiting the unique capabilities of fiber-optic sensors—such as distributed acoustic sensing (DAS)—to provide continuous, high-resolution observations across extensive spatial domains. These sensors transform standard telecom fiber cables into large-scale arrays capable of detecting subtle changes in ground motion, temperature, and strain.
Dr. Biondi’s research encompasses a variety of applications, including monitoring seismic activity, mapping subsurface fluid movement, and assessing the impacts of environmental changes such as volcanic intrusions or groundwater flow. By collecting and analyzing massive datasets from fiber-optic arrays deployed in urban, natural, and engineered environments, he develops algorithms and modeling methods to extract information about processes that were previously challenging to observe with traditional point sensors.
This work directly impacts our ability to detect and respond to natural hazards, manage water resources, and understand long-term environmental trends. His novel approaches support early warning systems for earthquakes and infrastructure failures and enable more sustainable management of natural resources. Applying cutting-edge machine learning and signal processing, Dr. Biondi’s team refines interpretation of fiber-sensing data, revealing the nuanced interactions within the Earth’s subsurface and surface environments.
Collaboration is a central theme, with partnerships spanning academia, industry, and governmental agencies. His group develops open-source tools and datasets to facilitate broader adoption of fiber-optic sensing in Earth science research. Dr. Biondi frequently publishes and presents findings at international conferences, aiming to inspire innovation in the use of unconventional sensing networks for environmental monitoring.
Ultimately, the work seeks to transform our capacity to observe and understand complex, multiscale Earth system processes by making sensing more accessible, scalable, and informative. This next-generation approach to geophysical monitoring promises profound impacts on hazard mitigation, resource management, and environmental stewardship.
2025-26 Courses
- Computational Earth System Analysis
GEOPHYS 245 (Spr) - Fiber Sensing
GEOPHYS 385F (Aut, Win, Spr) -
Independent Studies (3)
- Honors Program
GEOPHYS 198 (Aut, Spr) - Research in Geophysics
GEOPHYS 400 (Aut, Win, Spr) - Undergraduate Research in Geophysics
GEOPHYS 196 (Aut, Win, Spr)
- Honors Program
Stanford Advisees
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Doctoral Dissertation Advisor (AC)
Alina Belyalova
All Publications
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Minute-scale dynamics of recurrent dike intrusions in Iceland with fiber-optic geodesy.
Science (New York, N.Y.)
2025: eadu0225
Abstract
Continuous geodetic measurements near volcanic systems can image magma transport dynamics, yet resolving dike intrusions with high spatiotemporal resolution remains challenging. We introduce fiber-optic geodesy, leveraging low-frequency distributed acoustic sensing (LFDAS) recordings along a telecommunication fiber-optic cable, to track dike intrusions near Grindavík, Iceland, on a minute timescale. LFDAS reveals distinct strain responses from nine intrusive events, six resulting in fissure eruptions. Geodetic inversion of LFDAS strain reveals detailed magmatic intrusions, with inferred dike volume rate peaking systematically 15 to 22 min before the onset of each eruption. Our results demonstrate DAS's potential for a dense strainmeter array, enabling high-resolution, nearly real-time imaging of subsurface quasi-static deformations. In active volcanic regions, LFDAS recordings can offer critical insights into magmatic evolution, eruption forecasting, and hazard assessment.
View details for DOI 10.1126/science.adu0225
View details for PubMedID 40273283
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Fiber-optic seismic sensing of vadose zone soil moisture dynamics.
Nature communications
2024; 15 (1): 6432
Abstract
Vadose zone soil moisture is often considered a pivotal intermediary water reservoir between surface and groundwater in semi-arid regions. Understanding its dynamics in response to changes in meteorologic forcing patterns is essential to enhance the climate resiliency of our ecological and agricultural system. However, the inability to observe high-resolution vadose zone soil moisture dynamics over large spatiotemporal scales hinders quantitative characterization. Here, utilizing pre-existing fiber-optic cables as seismic sensors, we demonstrate a fiber-optic seismic sensing principle to robustly capture vadose zone soil moisture dynamics. Our observations in Ridgecrest, California reveal sub-seasonal precipitation replenishments and a prolonged drought in the vadose zone, consistent with a zero-dimensional hydrological model. Our results suggest a significant water loss of 0.25 m/year through evapotranspiration at our field side, validated by nearby eddy-covariance based measurements. Yet, detailed discrepancies between our observations and modeling highlight the necessity for complementary in-situ validations. Given the escalated regional drought risk under climate change, our findings underscore the promise of fiber-optic seismic sensing to facilitate water resource management in semi-arid regions.
View details for DOI 10.1038/s41467-024-50690-6
View details for PubMedID 39103375
View details for PubMedCentralID PMC11300608
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Seismic arrival-time picking on distributed acoustic sensing data using semi-supervised learning.
Nature communications
2023; 14 (1): 8192
Abstract
Distributed Acoustic Sensing (DAS) is an emerging technology for earthquake monitoring and subsurface imaging. However, its distinct characteristics, such as unknown ground coupling and high noise level, pose challenges to signal processing. Existing machine learning models optimized for conventional seismic data struggle with DAS data due to its ultra-dense spatial sampling and limited manual labels. We introduce a semi-supervised learning approach to address the phase-picking task of DAS data. We use the pre-trained PhaseNet model to generate noisy labels of P/S arrivals in DAS data and apply the Gaussian mixture model phase association (GaMMA) method to refine these noisy labels and build training datasets. We develop PhaseNet-DAS, a deep learning model designed to process 2D spatio-temporal DAS data to achieve accurate phase picking and efficient earthquake detection. Our study demonstrates a method to develop deep learning models for DAS data, unlocking the potential of integrating DAS in enhancing earthquake monitoring.
View details for DOI 10.1038/s41467-023-43355-3
View details for PubMedID 38081845
View details for PubMedCentralID PMC10713581
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An upper-crust lid over the Long Valley magma chamber.
Science advances
2023; 9 (42): eadi9878
Abstract
Geophysical characterization of calderas is fundamental in assessing their potential for future catastrophic volcanic eruptions. The mechanism behind the unrest of Long Valley Caldera in California remains highly debated, with recent periods of uplift and seismicity driven either by the release of aqueous fluids from the magma chamber or by the intrusion of magma into the upper crust. We use distributed acoustic sensing data recorded along a 100-kilometer fiber-optic cable traversing the caldera to image its subsurface structure. Our images highlight a definite separation between the shallow hydrothermal system and the large magma chamber located at ~12-kilometer depth. The combination of the geological evidence with our results shows how fluids exsolved through second boiling provide the source of the observed uplift and seismicity.
View details for DOI 10.1126/sciadv.adi9878
View details for PubMedID 37851798
View details for PubMedCentralID PMC10584340
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The break of earthquake asperities imaged by distributed acoustic sensing.
Nature
2023; 620 (7975): 800-806
Abstract
Rupture imaging of megathrust earthquakes with global seismic arrays revealed frequency-dependent rupture signatures1-4, but the role of high-frequency radiators remains unclear3-5. Similar observations of the more abundant crustal earthquakes could provide critical constraints but are rare without ultradense local arrays6,7. Here we use distributed acoustic sensing technology8,9 to image the high-frequency earthquake rupture radiators. By converting a 100-kilometre dark-fibre cable into a 10,000-channel seismic array, we image four high-frequency subevents for the 2021 Antelope Valley, California, moment-magnitude 6.0 earthquake. After comparing our results with long-period moment-release10,11 and dynamic rupture simulations, we suggest that the imaged subevents are due to the breaking of fault asperities-stronger spots or pins on the fault-that substantially modulate the overall rupture behaviour. An otherwise fading rupture propagation could be promoted by the breaking of fault asperities in a cascading sequence. This study highlights how we can use the extensive pre-existing fibre networks12 as high-frequency seismic antennas to systematically investigate the rupture process of regional moderate-sized earthquakes. Coupled with dynamic rupture modelling, it could improve our understanding of earthquake rupture dynamics.
View details for DOI 10.1038/s41586-023-06227-w
View details for PubMedID 37532935
View details for PubMedCentralID 3606976
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Earthquake focal mechanisms with distributed acoustic sensing.
Nature communications
2023; 14 (1): 4181
Abstract
Earthquake focal mechanisms provide critical in-situ insights about the subsurface faulting geometry and stress state. For frequent small earthquakes (magnitude< 3.5), their focal mechanisms are routinely determined using first-arrival polarities picked on the vertical component of seismometers. Nevertheless, their quality is usually limited by the azimuthal coverage of the local seismic network. The emerging distributed acoustic sensing (DAS) technology, which can convert pre-existing telecommunication cables into arrays of strain/strain-rate meters, can potentially fill the azimuthal gap and enhance constraints on the nodal plane orientation through its long sensing range and dense spatial sampling. However, determining first-arrival polarities on DAS is challenging due to its single-component sensing and low signal-to-noise ratio for direct body waves. Here, we present a data-driven method that measures P-wave polarities on a DAS array based on cross-correlations between earthquake pairs. We validate the inferred polarities using the regional network catalog on two DAS arrays, deployed in California and each comprising ~ 5000 channels. We demonstrate that a joint focal mechanism inversion combining conventional and DAS polarity picks improves the accuracy and reduces the uncertainty in the focal plane orientation. Our results highlight the significant potential of integrating DAS with conventional networks for investigating high-resolution earthquake source mechanisms.
View details for DOI 10.1038/s41467-023-39639-3
View details for PubMedID 37443136
View details for PubMedCentralID PMC10345142
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Properties of a deep seismic waveguide measured with an optical fiber
PHYSICAL REVIEW RESEARCH
2021; 3 (1)
View details for DOI 10.1103/PhysRevResearch.3.013164
View details for Web of Science ID 000620022200002
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ADAPTATION OF A RANGE-DOPPLER ALGORITHM TO MULTISTATIC SIGNALS FROM ULTRASOUND ARRAYS
IEEE. 2021: 3269-3272
View details for DOI 10.1109/IGARSS47720.2021.9554158
View details for Web of Science ID 001250139803111
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Estimating Signal and Structured Noise in Ultrasound Data using Prediction-Error Filters
edited by Byram, B. C., Ruiter, N. V.
SPIE-INT SOC OPTICAL ENGINEERING. 2019
View details for DOI 10.1117/12.2513514
View details for Web of Science ID 000471826100024
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Nonstretch normal moveout through iterative partial correction and deconvolution.
Geophysics
2014; 79 (4): V131-V141
View details for DOI 10.1190/geo2013-0392.1
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Non-Stretch Fourth Order NMO through Iterative Partial Corrections and Deconvolution
75th EAGE Conference & Exhibition incorporating SPE EUROPEC 2013
2013
View details for DOI 10.3997/2214-4609.20130020
https://orcid.org/0000-0002-3305-0982