Received wisdom about the main driver of the South Asian monsoon comes into question with a report that tests the idea that the Himalayas, not the Tibetan plateau, are the essential topographic ingredient.
References
Boos, W. R. & Kuang, Z. Nature 463, 218–222 (2010).
Gadgil, S. Annu. Rev. Earth Planet. Sci. 31, 429–467 (2003).
Sarachik, E. S. Dyn. Atmos. Oceans 2, 455–469 (1978).
Emanuel, K. A., Neelin, J. D. & Bretherton, C. S. Q. J. R. Metereol. Soc. 120, 1111–1143 (1994).
Chakraborty, A., Nanjundiah, R. & Srinivasan, J. Ann. Geophys. 24, 2075–2089 (2006).
Ashfaq, M. et al. Geophys. Res. Lett. 36, doi:10.1029/2008GL036500 (2009).
Blanford, H. F. Mem. India Meteorol. Dep. 2, 217–448 (1886).
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Cane, M. A moist model monsoon. Nature 463, 163–164 (2010). https://doi.org/10.1038/463163a
Published:
Issue Date:
DOI: https://doi.org/10.1038/463163a
- Springer Nature Limited
This article is cited by
-
Understanding the Asian summer monsoon onset in terms of catastrophe theory
Theoretical and Applied Climatology (2019)
-
Changes in Indian Summer Monsoon Using Neodymium (Nd) Isotopes in the Andaman Sea During the Last 24,000 years
Earth Systems and Environment (2019)