Articles | Volume 18, issue 10
https://doi.org/10.5194/tc-18-4547-2024
https://doi.org/10.5194/tc-18-4547-2024
Research article
 | 
02 Oct 2024
Research article |  | 02 Oct 2024

A model framework for atmosphere–snow water vapor exchange and the associated isotope effects at Dome Argus, Antarctica – Part 1: The diurnal changes

Tianming Ma, Zhuang Jiang, Minghu Ding, Pengzhen He, Yuansheng Li, Wenqian Zhang, and Lei Geng

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Cited articles

An, C., Hou, S., Jiang, S., Li, Y., Ma, T., Curran, M. A. J., Pang, H., Zhang, Z., Zhang, W., Yu, J., Liu, K., Shi, G., Ma, H., and Sun, B.: The long-term cooling trend in East Antarctic Plateau over the past 2000 years is only robust between 550 and 1550 CE, Geophys. Res. Lett., 48, e2021GL092923, https://doi.org/10.1029/2021GL092923, 2021. 
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Short summary
We constructed a box model to evaluate the isotope effects of atmosphere–snow water vapor exchange at Dome A, Antarctica. The results show clear and invisible diurnal changes in surface snow isotopes under summer and winter conditions, respectively. The model also predicts that the annual net effects of atmosphere–snow water vapor exchange would be overall enrichments in snow isotopes since the effects in summer appear to be greater than those in winter at the study site.