Patagonian Ice Sheet shaped regional climate during the Last Glacial Maximum

During the Last Glacial Maximum, changes in the thickness of the Patagonian Ice Sheet modified southern Andean topography. However, the resulting atmospheric feedbacks remain poorly constrained. Using an atmosphere–land coupled model, we isolated the climate response to prescribed ice-sheet thicknesses. Our results indicate that a thicker ice sheet generates a decrease in low level zonal winds, a westward shift in precipitation, a temperature increase along the western margin of Eastern Patagonia, and an increase in storm activity over Patagonia. A decrease in thickness generates the opposite pattern. Our findings suggest that the Patagonian Ice Sheet not only responded to climate change, but also actively modulated it—highlighting the role of topographic forcing in shaping atmospheric circulation over the Southern Hemisphere mid-latitudes. The Patagonian ice sheet not only responded to climate change but also actively influenced it regionally, highlighting the role of topographic forcing in shaping atmospheric circulation during glacial-interglacial cycles, according to a modeling study.

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Publication Details

Journal
Communications Earth & Environment
Published
2025-10-08
DOI
https://doi.org/10.1038/s43247-025-02762-8
Citations
1
Primary Topic
Geology and Paleoclimatology Research
Type
article
Field-Weighted Citation Impact
1.30

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article

Patagonian Ice Sheet shaped regional climate during the Last Glacial Maximum

Nicolás J. Cosentino, Álvaro Gómez-Contreras, Fabrice Lambert, Summer Rupper et al.
1 citations
Communications Earth & Environment
Geology and Paleoclimatology Research
1.30
article

Patagonian Ice Sheet shaped regional climate during the Last Glacial Maximum

Nicolás J. Cosentino, Álvaro Gómez-Contreras, Fabrice Lambert, Summer Rupper, Jiang Zhu, Esteban A. Sagredo, Fabian M. Riquelme-Barraza, María José Puentes-Nazal
article en
1 citations

Abstract

During the Last Glacial Maximum, changes in the thickness of the Patagonian Ice Sheet modified southern Andean topography. However, the resulting atmospheric feedbacks remain poorly constrained. Using an atmosphere–land coupled model, we isolated the climate response to prescribed ice-sheet thicknesses. Our results indicate that a thicker ice sheet generates a decrease in low level zonal winds, a westward shift in precipitation, a temperature increase along the western margin of Eastern Patagonia, and an increase in storm activity over Patagonia. A decrease in thickness generates the opposite pattern. Our findings suggest that the Patagonian Ice Sheet not only responded to climate change, but also actively modulated it—highlighting the role of topographic forcing in shaping atmospheric circulation over the Southern Hemisphere mid-latitudes. The Patagonian ice sheet not only responded to climate change but also actively influenced it regionally, highlighting the role of topographic forcing in shaping atmospheric circulation during glacial-interglacial cycles, according to a modeling study.

Communications Earth & EnvironmentVol. 6(1)
NSF National Center for Atmospheric Research (US), Consejo Nacional de Investigaciones Científicas y Técnicas (AR), Pontificia Universidad Católica de Chile (CL), University of Utah (US), Universidad de Buenos Aires (AR), Center for Climate and Resilience Research (CL), Instituto Franco-Argentino sobre Estudios de Clima y sus Impactos (AR), Fundación Ciencias Exactas y Naturales (AR), University of Chile (CL)
National Science Foundation, Agencia Nacional de Investigación y Desarrollo, Fondo de Financiamiento de Centros de Investigación en Áreas Prioritarias
Openalex Percentile: Top 17%
Geology and Paleoclimatology Research
1.30
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