Earth Surf. Dynam., 6, 351–367, 2018 https://doi.org/10.5194/esurf-6-351-2018 © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. Seismic signature of turbulence during the 2017 Oroville Dam spillway erosion crisis Phillip J. Goodling, Vedran Lekic, and Karen Prestegaard Department of Geology, University of Maryland, College Park, MD 20742, USA Correspondence: Phillip J. Goodling (
[email protected]) Received: 9 December 2017 – Discussion started: 2 January 2018 Revised: 5 April 2018 – Accepted: 8 April 2018 – Published: 9 May 2018 Abstract. Knowing the location of large-scale turbulent eddies during catastrophic flooding events improves predictions of erosive scour. The erosion damage to the Oroville Dam flood control spillway in early 2017 is an example of the erosive power of turbulent flow. During this event, a defect in the simple concrete channel quickly eroded into a 47 m deep chasm. Erosion by turbulent flow is difficult to evaluate in real time, but near-channel seismic monitoring provides a tool to evaluate flow dynamics from a safe distance. Previous studies have had limited ability to identify source location or the type of surface wave (i.e., Love or Rayleigh wave) excited by different river processes. Here we use a single three-component seismometer method (frequency-dependent po- larization analysis) to characterize the dominant seismic source location and seismic surface waves produced by the Oroville Dam flood control spillway, using the abrupt change in spillway geometry as a natural experiment. We find that the scaling exponent between seismic power and release discharge is greater following damage to the spillway, suggesting additional sources of turbulent energy dissipation excite more seismic energy.