Articles | Volume 5, issue 3
https://doi.org/10.5194/wcd-5-1137-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/wcd-5-1137-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Spatial and temporal variability of the freezing level in Patagonia's atmosphere
Glaciología y Cambio Climático, Centro de Estudios Científicos (CECs), Valdivia, 5090000, Chile
Claudio Bravo
Glaciología y Cambio Climático, Centro de Estudios Científicos (CECs), Valdivia, 5090000, Chile
Álvaro Gónzalez-Reyes
Instituto de Ciencias de la Tierra (ICT), Facultad de Ciencias, Universidad Austral de Chile, Valdivia 5090000, Chile
Laboratorio de Dendrocronología y Cambio Global, Universidad Austral de Chile, Valdivia, 5090000, Chile
Centro de Humedales Río Cruces (CEHUM), Universidad Austral de Chile, Valdivia, 5090000, Chile
Centro de Investigación, Dinámica de Ecosistemas Marinos de Altas Latitudes (IDEAL), Universidad Austral de Chile, Valdivia, 5090000, Chile
Piero Mardones
Centro de Investigación en Ecosistemas de la Patagonia (CIEP), Coyhaique, 5950000, Chile
Editorial note: the supplement was replaced on 31 October 2024 as values in Table S1 were erroneous. This has now been corrected.
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Short summary
This study analyses the 0 °C isotherm in Patagonia from 1959 to 2021, using observational and fifth-generation European Centre for Medium-Range Weather Forecasts atmospheric reanalysis data. The model aligns well with observations, highlighting significant altitude variations between the western and eastern sides of the austral Andes, a correlation between isotherm fluctuations and the Southern Annular Mode index, and an upward trend in the study area (especially in northwestern Patagonia).
This study analyses the 0 °C isotherm in Patagonia from 1959 to 2021, using observational and...