“…An important byproduct of the sky-wave propagation mode used by SuperDARN radars is the occurrence of ground scatter (GS) echoes from land and ocean surfaces along the signal path. While these GS returns are often treated as noise when producing global maps of ionospheric plasma motion (Chisham & Pinnock, 2002), they can be useful for monitoring different geophysical phenomena such as trav-eling ionospheric disturbances (e.g., Bristow et al, 1996;He et al, 2004;Frissell et al, 2016), HF absorption caused by solar flares (e.g., Hosokawa et al, 2000;Chakraborty et al, 2018), or even land and ocean surface features (Shand et al, 1998;Ponomarenko et al, 2010;Greenwood et al, 2011).…”