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- W1548063599 abstract "[1] To improve our understanding of paleoclimatic records in the southwest Yukon, we examined controls on precipitation δ18O using an isotopically-equipped atmospheric general circulation model (GCM). Our results show that, particularly during the cool-season, elevated δ18O is associated with a deeper Aleutian Low and stronger southerly moisture flow, while lower δ18O is associated with the opposite meteorological conditions. These results suggest that the large mid-19th century shift towards lower δ18O values seen in paleoclimate records from the region was associated with a shift towards a weaker Aleutian Low. While in disagreement with a previous interpretation of this shift, it is consistent with records of glacial advance and tree-ring growth during the same period, and observational studies of Aleutian Low controls on temperature and precipitation in the region." @default.
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- W1548063599 date "2010-03-01" @default.
- W1548063599 modified "2023-10-16" @default.
- W1548063599 title "A GCM-based analysis of circulation controls on<i>δ</i><sup>18</sup>O in the southwest Yukon, Canada: Implications for climate reconstructions in the region" @default.
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- W1548063599 doi "https://doi.org/10.1029/2009gl041408" @default.
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