AGU 2023

Figure 1. An animation of timelapse electrical resistivity images at Government Gultch, Laramie, WY from April 20 to August 14, 2022.

Figure 2. An animation of change in water content derived from TLERT at Headquarters, Laramie Range, WY (Kotikain et al., 2019).

References

Kotikian, M., Parsekian, A. D., Paige, G., & Carey, A. (2019). Observing Heterogeneous Unsaturated Flow at the Hillslope Scale Using Time‐Lapse Electrical Resistivity Tomography. Vadose Zone Journal, 18(1), 1-16. https://doi.org/10.2136/vzj2018.07.0138

Pleasants, M. S., Kelleners, T. J., Parsekian, A. D., & Befus, K. M. (2023). A comparison of hydrological and geophysical calibration data in layered hydrologic models of mountain hillslopes. Water Resources Research, 59, e2022WR033506. https://doi.org/10.1029/2022WR033506 

Pope, G.G., Nyquist, J.E., & Toran, L. (2022). Time-Lapse Resistivity Monitoring of a Simulated Runoff Test in a Bioswale, Philadelphia. Journal of Sustainable Water in the Built Environment, 9(1). https://doi.org/10.1061/JSWBAY.0001003

Yonesha, D., Milewski, A., Parsekian, A., Rasmussen, T.C., & Garing, C. (2023). A Geophysical Approach to Monitor Infiltration and Geochemical Processes in an Arid and Saline Environment. AGU, H31E-05. https://agu.confex.com/agu/fm23/meetingapp.cgi/Paper/1372119