Influence of seasonal sea-ice loss on Arctic precipitation δ18O: a GCM-based analysis of monthly data

• Published in: Polar research Vol. 42; pp. 1 - 13
• Main Authors: Song, Wenxuan, Liu, Zhongfang, Lan, Haimao, Huan, Xiaohe
• Format: Journal Article
• Language: English
• Published: Spånga Open Academia 08.12.2023; Norwegian Polar Institute
• Subjects: Ablation; Air temperature; arctic warming; Atmospheric circulation; Environmental tracers; Evaporation; General circulation models; Hydrologic cycle; Hydrological cycle; Hydrology; Isotopes; local evaporation; Palaeotemperature; palaeotemperature reconstruction; Performance evaluation; Precipitation; precipitation isotope; Sea ice; Simulation; Summer; Temperature effects; Tracers; Winter; Beaufort Sea; Arctic region
• ISSN: 0800-0395; 1751-8369
• DOI: 10.33265/polar.v42.9751

Rapid Arctic warming and sea ice loss have led to an intensification of the Arctic hydrological cycle, which is characterized by increased local evaporation and precipitation. Stable water isotopes as environmental tracers can provide useful insights into the Arctic hydrological cycle. However, the paucity of isotopic observations in the Arctic has limited our understanding of the hydrological changes. Here, we use an isotope-enabled atmospheric general circulation model (IsoGSM) combined with the Global Network of Isotopes in Precipitation (GNIP) observations to investigate the relationship between sea ice changes and Arctic precipitation d18O (d18Op), and reveal the relative influence of local air temperature and evaporation on Arctic summer and winter d18Op. We find that the Arctic d18Op is negatively correlated with sea ice concentration, but positively with air temperature. Sea ice loss leads to enriched Arctic d18Op through enhanced local evaporation and warming, but the relative importance of these processes varies between seasons. During summer, both local evaporation and warming contribute equally to d18Opchanges. In contrast, winter δ18O is predominantly driven by air temperature. This work improves our understanding of how Arctic precipitation isotopes respond to sea ice changes and has implications for the Arctic hydrological cycle and paleotemperature reconstructions.