Over the past two months, I’ve been deeply engaged in understanding our work’s fundamentals and context, often seeking guidance from John, my principal investigator. I’ve also been analyzing data from two events in Arroyo de los Pinos (ADLP), New Mexico, on August 10th, 2023, and July 5th, 2021. Unfortunately, the ECM (Electromagnetic Current Meter) was damaged during both incidents, limiting data availability to just 5 to 8 minutes per event. Despite setbacks, I find the ECM data more intriguing than seismic data. As an engineer, I’ve explored ECM’s principles and discovered that its velocity component doesn’t precisely reflect actual velocity, but rather the rotational component. This has piqued my curiosity about its correlation with Turbulent Kinetic Energy (TKE). Although establishing correlations with other parameters has been challenging, I remain dedicated. Awaiting instrument deployment consumes a significant portion of my time, along with anticipation for an upcoming collaborative experiment at the end of next month with the University of Texas, Austin, and New Mexico Tech.