Multi-year time series of H<sub>2sub> and δD(H<sub>2sub>) were measured at a regional tall tower site.
The dataset contains the first measured δD height profiles in the boundary layer.
The features of the time series are consistent with large anthropogenic influences.
The apparent δD source signature is much lower than fossil fuel combustion estimates.
Both source signature and profiles suggest microbial H<sub>2sub> production around the tower.