Southern hemisphere forced millennial scale Indian summer monsoon variability during the late Pleistocene

Peninsular India hosts the initial rain-down of the Indian Summer Monsoon (ISM) after which winds travel further east inwards into Asia. Stalagmite oxygen isotope composition from this region, such as those from Belum Cave, preserve the vital signals of the past ISM variability. These archives exper...

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Detalles Bibliográficos
Autores principales: Band, Shraddha T., Yadava, M. G., Kaushal, Nikita, Midhun, M., Thirumalai, Kaustubh, Francis, Timmy, Laskar, Amzad, Ramesh, R., Henderson, Gideon M., Narayana, A. C.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2022
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9203564/
https://www.ncbi.nlm.nih.gov/pubmed/35710914
http://dx.doi.org/10.1038/s41598-022-14010-6

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9203564/
https://www.ncbi.nlm.nih.gov/pubmed/35710914
http://dx.doi.org/10.1038/s41598-022-14010-6

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