This study investigates the concentrations and
δ
15
N values of NH
3
in Beijing during
and after the 2020 COVID-19 lockdown. Higher NH
3
concentrations and lower
δ
15
N-NH
3(measured)
were
observed at most sites in 2020 compared to 2017. Except for a
site inside a tunnel, NH
3
concentrations did not
increase significantly after the lockdown had ended compared to
those during the lockdown, while
δ
15
N-NH
3(measured)
increased
by 2.1–9.9‰. Nonagricultural sources (fossil fuel
and urban waste) overall contributed 81% and 62% of
NH
3
at on-road (tunnel interior) and nonroad
(CAU) sites in 2020, respectively, comparable to those in 2017
(without significant difference). The contribution of
nonagricultural sources slightly increased after the lockdown
compared to the contribution during the lockdown at the nonroad
site and hardly changed at the tunnel interior site. Our results
suggest that (1) unfavorable meteorological conditions,
especially lower boundary layer heights and changes in regional
transport patterns, might play a more important role than
reduced anthropogenic emissions in the temporal variations of
Beijing NH
3
and (2) the effect of reduced
anthropogenic emissions, during the COVID-19 outbreak or with
the future implementation of emission control strategies, on
atmospheric NH
3
can be better demonstrated by
isotope-based source apportionment of NH
3
, rather
than only by changes in NH
3
concentrations.