The Tibetan Plateau plays a central role in global atmospheric circulation, acts as a key biodiversity hotspot, and delivers fresh water for more than 20% of the global population. Projecting its future uplift and erosion trajectory over geological time can offer potential testable hypotheses into interactions between tectonic and surface processes.
This is a preview of subscription content, access via your institution
Relevant articles
Open Access articles citing this article.
-
Physiography, foraging mobility, and the first peopling of Sahul
Nature Communications Open Access 23 April 2024
Access options
Access Nature and 54 other Nature Portfolio journals
Get Nature+, our best-value online-access subscription
$29.99 / 30 days
cancel any time
Subscribe to this journal
Receive 12 digital issues and online access to articles
$99.00 per year
only $8.25 per issue
Buy this article
- Purchase on Springer Link
- Instant access to full article PDF
Prices may be subject to local taxes which are calculated during checkout
References
Molnar, P., England, P. & Martinod, J. Mantle dynamics, uplift of the Tibetan Plateau and the Indian monsoon. Rev. Geophys. 31, 357–396 (1993).
Raymo, M. E. & Ruddiman, W. F. Tectonic forcing of late Cenozoic climate. Nature 359, 117–122 (1992).
Liu, X. et al. Continental drift and plateau uplift control origination and evolution of Asian and Australian monsoons. Sci. Rep. 7, 40344 (2017).
Ding, L. et al. Timing and mechanisms of Tibetan Plateau uplift. Nat. Rev. Earth. Environ. https://doi.org/10.1038/s43017-022-00318-4 (2022).
Hallet, B. & Molnar, P. Distorted drainage basins as markers of crustal strain east of the Himalayas. J. Geophys. Res. 106, 13697–13709 (2001).
Clift, P. & Blusztajn, J. Reorganization of the western Himalayan River system after five million years ago. Nature 438, 1001–1003 (2005).
Yoshida, M. & Hamano, Y. Pangea breakup and northward drift of the Indian subcontinent reproduced by numerical model of mantle convection. Sci. Rep. 5, 8407 (2015).
Yuan, X. P. et al. Propagating uplift controls on high-elevation, low-relief landscape formation in the southeast Tibetan Plateau. Geology 50, 60–65 (2021).
Becker, M. et al. Water level changes, subsidence, and sea level rise in the Ganges–Brahmaputra–Meghna delta. PNAS 117, 201912921 (2021).
Author information
Authors and Affiliations
Contributions
The authors contributed equally to all aspects of the article.
Corresponding author
Ethics declarations
Competing interests
The authors declare no competing interests.
Additional information
Publisher’s Note
Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
Supplementary Information
Rights and permissions
About this article
Cite this article
Rey, P.F., Salles, T., Zahirovic, S. et al. A glimpse into a possible geomorphic future of Tibet. Nat Rev Earth Environ 3, 613–615 (2022). https://doi.org/10.1038/s43017-022-00355-z
Published:
Issue Date:
DOI: https://doi.org/10.1038/s43017-022-00355-z
This article is cited by
-
Physiography, foraging mobility, and the first peopling of Sahul
Nature Communications (2024)