Three decades of meteorological observations show that Himalayan glaciers have been cooling because of intensified downslope winds, in contrast to the warming observed elsewhere in the region.
References
Scherler, D., Bookhagen, B. & Strecker, M. R. Nat. Geosci. 4, 156–159 (2011).
Bolch, T. et al. Science 336, 310–314 (2012).
Salerno, F. et al. Nat. Geosci. https://doi.org/10.1038/s41561-023-01331-y (2023).
Bookhagen, B. & Burbank, D. W. J. Geophys. Res. 115, F03019 (2010).
Barros, A. P. & Lang, T. J. Mon. Weath. Rev. 131, 1408–1427 (2003).
Ueno, K., Toyotsu, K., Bertolani, L. & Tartari, G. Mon. Weath. Rev. 136, 2507–2522 (2008).
Norris, J. et al. Clim. Dyn. 49, 2179–2204 (2017).
Hewitt, K. Mountain Res. Dev. 25, 332–340 (2005).
Norris, J. et al. npj Clim. Atmos. Sci. 3, 1 (2020).
Author information
Authors and Affiliations
Corresponding author
Ethics declarations
Competing interests
The author declares no competing interests.
Rights and permissions
About this article
Cite this article
Norris, J. Cooling Himalayan glaciers. Nat. Geosci. 16, 1076–1077 (2023). https://doi.org/10.1038/s41561-023-01344-7
Published:
Issue Date:
DOI: https://doi.org/10.1038/s41561-023-01344-7
- Springer Nature Limited