ArticleNature communications2021
Tectonic and climatic drivers of Asian monsoon evolution.
Article in Nature communications, 2021. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 8 papers.
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Who cites it
8 citing papers in PubMed.
- East Asian climate evolution during the Cenozoic: A review from the modeling perspective.Fundamental research · 2025Review
- Late Cenozoic river reorganization related to tectonic extrusion formed the modern drainage system in southeastern Tibet.Proceedings of the National Academy of Sciences of the United States of America · 2025Article
- The role of the North American continent in strengthening the Asian summer monsoon.Science advances · 2025Article
- Miocene African topography induces decoupling of Somali Jet and South Asian summer monsoon rainfall.Nature communications · 2025Article
- Vegetation feedbacks accelerated the late Miocene climate transition.Science advances · 2025Article
- Tectonic and orbital forcing of the South Asian monsoon in central Tibet during the late Oligocene.Proceedings of the National Academy of Sciences of the United States of America · 2023Article
- Weakening of the South Asian summer monsoon linked to interhemispheric ice-sheet growth since 12 Ma.Nature communications · 2023Article
- Late Miocene Leaves and Endocarps ofBiology · 2022Article
Corrections and comments
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Authors and funding
6 authors.
Funding
No grant is acknowledged in the PubMed record.
Abstract
Asian Monsoon rainfall supports the livelihood of billions of people, yet the relative importance of different drivers remains an issue of great debate. Here, we present 30 million-year model-based reconstructions of Indian summer monsoon and South East Asian monsoon rainfall at millennial resolution. We show that precession is the dominant direct driver of orbital variability, although variability on obliquity timescales is driven through the ice sheets. Orographic development dominated the evolution of the South East Asian monsoon, but Indian summer monsoon evolution involved a complex mix of contributions from orography (39%), precession (25%), atmospheric CO
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