Abstract
Abstract. The estimation of radon progeny in the Arctic region represents
a scientific challenge due to the required low limit of detection in
consideration of the limited radon emanation associated with permafrost
dynamics. This preliminary study highlighted, for the first time above
70∘ N, the possibility to monitor radon progeny in the Arctic region
with a higher time resolution. The composition of the radon progeny offered
the opportunity to identify air masses dominated by long-range transport, in
presence or absence of near-constant radon progeny instead of long- and short-lived progenies. Furthermore, the different ratio between radon and thoron progenies evidenced the contributions of local emissions and atmospheric
stability. Two different emanation periods were defined in accordance with the
permafrost dynamics at the ground and several accumulation windows were
recognized coherently to the meteo-climatic conditions occurring at the study
site.
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