nerc.ac.uk

Thin and ephemeral snow shapes melt and runoff dynamics in the Peruvian Andes

Fyffe, Catriona L. ORCID: https://orcid.org/0000-0001-6950-3501; Potter, Emily ORCID: https://orcid.org/0000-0001-5273-1292; Miles, Evan ORCID: https://orcid.org/0000-0001-5446-8571; Shaw, Thomas E.; McCarthy, Michael ORCID: https://orcid.org/0000-0002-4138-0578; Orr, Andrew ORCID: https://orcid.org/0000-0001-5111-8402; Loarte, Edwin ORCID: https://orcid.org/0000-0003-3123-1904; Medina, Katy; Fatichi, Simone ORCID: https://orcid.org/0000-0003-1361-6659; Hellström, Rob; Baraer, Michel ORCID: https://orcid.org/0000-0003-4138-3354; Mateo, Emilio ORCID: https://orcid.org/0000-0003-3890-2707; Cochachin, Alejo; Westoby, Matthew ORCID: https://orcid.org/0000-0002-2070-5580; Pellicciotti, Francesca. 2025 Thin and ephemeral snow shapes melt and runoff dynamics in the Peruvian Andes. Communications Earth & Environment, 6, 434. 12, pp. 10.1038/s43247-025-02379-x

Before downloading, please read NORA policies.
[thumbnail of Open Access]
Preview
Text (Open Access)
© The Author(s) 2025.
s43247-025-02379-x.pdf - Published Version
Available under License Creative Commons Attribution Non-commercial 4.0.

Download (3MB) | Preview

Abstract/Summary

The snow and glaciers of the Peruvian Andes provide vital water supplies in a region facing water scarcity and substantial glacier change. However, there remains a lack of understanding of snow processes and quantification of the contribution of melt to runoff. Here we apply a distributed glacio-hydrological model over the Rio Santa basin to disentangle the role of the cryosphere in the Andean water cycle. Only at the highest elevations (>5000 m a.s.l.) is the snow cover continuous; at lower elevations, the snowpack is thin and ephemeral, with rapid cycles of snowfall and melt. Due to the large catchment area affected by ephemeral snow, its contribution to catchment inputs is substantial (23% and 38% in the wet and dry season, respectively). Ice melt is crucial in the mid-dry season (up to 44% of inputs). Our results improve estimates of water fluxes and call for further process-based modelling across the Andes.

Item Type: Publication - Article
Digital Object Identifier (DOI): 10.1038/s43247-025-02379-x
ISSN: 2662-4435
Additional Keywords: Climate change, Cryospheric science, Hydrology
Date made live: 09 Jun 2025 09:41 +0 (UTC)
URI: https://nora.nerc.ac.uk/id/eprint/539535

Actions (login required)

View Item View Item

Document Downloads

Downloads for past 30 days

Downloads per month over past year

More statistics for this item...