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Contribution of the Southern Annular Mode to variations in water isotopes of daily precipitation at Dome Fuji, East Antarctica
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  • Kanon Kino,
  • Atsushi Okazaki,
  • Alexandre Cauquoin,
  • Kei Yoshimura
Kanon Kino
Atmosphere and Ocean Research Institute, The University of Tokyo, Atmosphere and Ocean Research Institute, The University of Tokyo

Corresponding Author:[email protected]

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Atsushi Okazaki
Pennsylvania State University, Pennsylvania State University
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Alexandre Cauquoin
Institute of Industrial Science, The University of Tokyo, Institute of Industrial Science, The University of Tokyo
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Kei Yoshimura
University of Tokyo, University of Tokyo
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Abstract

Water isotopes measured in Antarctic ice cores enable reconstruction at the first order of the past temperature variations. However, the seasonality of the precipitation and episodic events, including synoptic-scale disturbances, influence the isotopic signals recorded in ice cores. In this study, we adopted an isotope-enabled atmospheric general circulation model from 1981 to 2010 to investigate variations in climatic factors in δ18O of precipitation (δ18Op) at Dome Fuji, East Antarctica. The Southern Annular Mode (SAM), the primary mode of atmospheric circulation in the southern mid-high latitudes, significantly contributes to the isotope signals. Positive δ18Op anomalies, especially in the austral winter, are linked to the negative polarity of the SAM, which weakens westerly winds and increases the southward inflow of water vapor flux. Daily variations in temperature and δ18Op in Dome Fuji are significantly small in the austral summer, and their contribution to the annual signals is limited. The isotope signals driven by the SAM are a locational feature of Dome Fuji, related to the asymmetric component of the large-scale atmospheric pattern.
16 Dec 2021Published in Journal of Geophysical Research: Atmospheres volume 126 issue 23. 10.1029/2021JD035397