In this paper we sampled ten different lakes in the Abisko region to evaluate spatial and temporal patterns of groundwater discharge and implications in lake CH4 emissions (1/6)
A 222Rn mass balance revealed that groundwater discharge was an important water source for the lakes, with inflows comparable to those from inlet streams (2/6).
Due to the high concentrations of CH4 in groundwater, groundwater inflows represent an important source of CH4 to these lakes, which can account for a large fraction of CH4 emissions (3/6).
The comparison of the magnitude of groundwater CH4 inputs to lakes with other potential CH4 sources and sinks evidences that groundwater discharge is a major mechanism controlling CH4 cycling the Arctic (4/6).
We also discuss spatial and temporal patterns of these fluxes. But I am not going to explain everything here! (5/6)