nedströmskällo

Nedströmskällo is a term used in hydrology and fluid dynamics that translates roughly from Swedish as "downstream source" or "downstream spring." It refers to a point within a watercourse where water emerges or becomes significantly more abundant from a source that is located downstream of the observation point. This contrasts with the more common understanding of a source being upstream.

Such a phenomenon can occur due to several geological or hydrological factors. One possibility is a complex underground aquifer system where water flows in unexpected directions, potentially resurfacing at a lower elevation. Another is the influence of subterranean tributaries or springs that feed into the main channel from below. In some cases, it could also be related to groundwater infiltration or even the release of stored water from natural reservoirs that are not immediately apparent.

Identifying a nedströmskällo is important for understanding the complete water balance of a river or stream. It can affect flow rate measurements, water quality assessments, and ecological studies by indicating a contribution to the water body that originates from a less intuitive location. The study of such sources requires detailed hydrogeological investigations and can reveal intricate connections within regional groundwater systems.