Articles | Volume 19, issue 5
https://doi.org/10.5194/tc-19-1897-2025
https://doi.org/10.5194/tc-19-1897-2025
Research article
 | 
19 May 2025
Research article |  | 19 May 2025

An unseasonal atmospheric river drives anomalous summer snow accumulation on glaciers of the subtropical Andes

Claudio Bravo, Sebastián Cisternas, Maximiliano Viale, Pablo Paredes, Deniz Bozkurt, and Nicolás García-Lee

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Cited articles

Adusumilli, S., Fish, M. A., Fricker, H. A., and Medley, B.: Atmospheric river precipitation contributed to rapid increases in surface height of the West Antarctic Ice Sheet in 2019, Geophys. Res. Lett., 48, e2020GL091076, https://doi.org/10.1029/2020GL091076, 2021. 
Alvarez-Garreton, C., Boisier, J. P., Garreaud, R., González, J., Rondanelli, R., Gayó, E., and Zambrano-Bigiarini, M.: HESS Opinions: The unsustainable use of groundwater conceals a “Day Zero”, Hydrol. Earth Syst. Sci., 28, 1605–1616, https://doi.org/10.5194/hess-28-1605-2024, 2024. 
Ayala, A., Pellicciotti, F., Peleg, N., and Burlando, P.: Melt and surface sublimation across a glacier in a dry environment: distributed energy-balance modelling of Juncal Norte Glacier, Chile, J. Glaciol., 63, 803–822, https://doi.org/10.1017/jog.2017.46, 2017. 
Ayala, Á., Farías-Barahona, D., Huss, M., Pellicciotti, F., McPhee, J., and Farinotti, D.: Glacier runoff variations since 1955 in the Maipo River basin, in the semiarid Andes of central Chile, The Cryosphere, 14, 2005–2027, https://doi.org/10.5194/tc-14-2005-2020, 2020. 
Barandun, M., Bravo, C., Grobety, B., Jenk, T., Fang, L., Naegeli, K., Rivera, A., Cisternas, S., Münster, T., and Schwikowski, M.: Anthropogenic influence on surface changes at the Olivares Glaciers; Central Chile, Sci. Total. Environ., 833, 155068, https://doi.org/10.1016/j.scitotenv.2022.155068, 2022. 
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Short summary
We analysed the impact of a summer snow accumulation event linked to an atmospheric river in central Chile. Using observational and remote sensing data, we show that accumulation prevails in all the glaciers of the Maipo River basin, and this sole event defines the fact that the Olivares Alfa glacier mass balance was close to equilibrium despite it being a dry year. This demonstrates that an unseasonal accumulation event can counteract the seasonal trends affecting subtropical Andean glaciers.
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