The rain shadow effect is prob somewhat exaggerated, but the Catoctins (while small) do rise sharply (so sharply that mountain biking national races have been held there). It’s an impressive little mountain chain. I drove through Gambrill today and there’s still snow up at the top and absolutely nothing at the bottom. It’s pretty wild. Obviously, the last snow was mostly due to elevation and likely not so much from upslope, but downsloping effects can be seen all year long as snow showers and tstorms sometimes fade as they sag south from the northwest…it’s a limited effect, but not non-existent imo.