Tropical mountain ice core δ(18)O: A Goldilocks indicator for global temperature change

Very high tropical alpine ice cores provide a distinct paleoclimate record for climate changes in the middle and upper troposphere. However, the climatic interpretation of a key proxy, the stable water oxygen isotopic ratio in ice cores (δ(18)O(ice)), remains an outstanding problem. Here, combining...

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Detalles Bibliográficos
Autores principales: Liu, Zhengyu, Bao, Yuntao, Thompson, Lonnie G., Mosley-Thompson, Ellen, Tabor, Clay, Zhang, Guang J., Yan, Mi, Lofverstrom, Marcus, Montanez, Isabel, Oster, Jessica
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2023
Materias:
Earth, Environmental, Ecological, and Space Sciences
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10631737/
https://www.ncbi.nlm.nih.gov/pubmed/37939192
http://dx.doi.org/10.1126/sciadv.adi6725

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10631737/
https://www.ncbi.nlm.nih.gov/pubmed/37939192
http://dx.doi.org/10.1126/sciadv.adi6725

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