Combining geoelectric field modelling and differential magnetometer data to validate GIC modelling in the UK High voltage power transmission grid
- British Geological Survey, Edinburgh, UK
Geomagnetically induced currents (GICs) have been identified as a hazard to the UK power grid and the security of electricity supply during severe geomagnetic storms. In order to monitor, model and forecast GICs, sophisticated models of the ground electric field and the network topology are required. We present a detailed analysis of differential magnetometer (DMM) and magnetotelluric (MT) data in the UK that allow the verification and validation of our network model for the UK power transmission grid. Combining the observation of line GICs measured with DMM in the past three years and the MT impedance tensor estimated at several locations in the UK shows an excellent fit of prediction and observation of GICs when using realistic modelled ground electric fields. This validates our whole network model allowing us to use it with confidence for real time and forecasting as well as extreme event analysis.
How to cite: Huebert, J., Beggan, C., Richardson, G., Gomez Perez, N., and Thomson, A.: Combining geoelectric field modelling and differential magnetometer data to validate GIC modelling in the UK High voltage power transmission grid, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-9495, https://doi.org/10.5194/egusphere-egu22-9495, 2022.