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I study why some volcanoes erupt with almost no warning while others swell for decades without erupting, and how to turn monitoring data into better eruption forecasts.

I am a volcano geophysicist at the University of Illinois Urbana-Champaign, where I completed my Ph.D. research with Prof. Patricia M. Gregg. I combine satellite radar (InSAR), GPS, earthquake records, finite-element models, and ensemble Kalman filter (EnKF) data assimilation to understand the magma systems of Okmok, Westdahl, and Veniaminof volcanoes in Alaska's Aleutian arc. My study of 'stealthy' eruptions at Veniaminof was covered by more than 30 news outlets worldwide.

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  1. Stealthy magma system behavior at Veniaminof Volcano, Alaska.

    Li, Y., Gregg, P. M., Lu, Z., & Wang, J.

    Frontiers in Earth Science, 13:1535083 (2025)

    Why a frequently erupting Alaskan volcano gives almost no warning. Covered by 30+ news outlets; Altmetric score in the top 1% of research outputs.

  2. The plausible relationship between deep long-period earthquakes and volatiles: a case study of the Alaska-Aleutian arc.

    McKee, K. F., Cauley, C., Rojas-Kolomiets, E., Li, Y., Hosseini, B., Daly, K., Ward, A., Roman, D. C., Wieser, P. E., Wallace, P. J., Fischer, T. P., Power, J. A., Plank, T., & Abers, G. A.

    Bulletin of Volcanology, 88:115 (2026)

    Deep earthquakes beneath Alaskan volcanoes occur at depths where gases come out of solution in magma.

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