Sibbald Fen is a beaver-structured wetland complex in the Rocky Mountain foothills that serves as our primary field laboratory for understanding how engineered hydrological networks function. Research here focuses on how beaver dams, canals, and ponds interact to regulate water storage, connectivity, and flow timing across interconnected landscapes, and how these hydrological changes propagate through the system. Using dense sensor networks, repeated UAV surveys and wildlife cameras, we quantify how water moves through beaver-modified systems and how changes in connectivity influence water quality, carbon dynamics, vegetation patterns, and wildlife use. A key goal is to identify the conditions under which hydrological connectivity reorganizes across space and time, and how these shifts cascade through broader ecosystem processes under a changing climate. Sibbald fen is a UNESCO Ecohydrology Demonstration Site located about 60 km west of Calgary.