The behaviour of water in the atmosphere is a poorly understood part of the hydrological cycle. Applying the principles of isotope chemistry to satellite data provides a powerful approach for improving the situation.
This is a preview of subscription content, access via your institution
Access options
Subscribe to this journal
Receive 51 print issues and online access
$199.00 per year
only $3.90 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
Worden, J. et al. Nature 445, 528–532 (2007).
Craig, H. Science 133, 1702–1703 (1961).
Lawrence, J. R. et al. J. Geophys. Res. 109, D06115 (2004).
Webster, C. R. & Heymsfeld, A. J. Science 302, 1742–1745 (2003).
Hanisco, T. F. et al. Geophys. Res. Lett. (in the press).
Irion, F. W. et al. Geophys. Res. Lett. 23, 2381–2384 (1996).
Moyer, E. J., Irion, F. W., Yung, Y. L. & Gunson, M. R. Geophys. Res. Lett. 23, 2385–2388 (1996).
Zakharov, V. I., Imasu, R., Gribanov, K. G., Hoffmann, G. & Jouzel, J. Geophys. Res. Lett. 31, L12104 (2004).
Dansgaard, W. Tellus 16, 436–468 (1964).
Rosenfeld, D. & Mintz, Y. J. Appl. Meteorol. 27, 209–215 (1988).
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Rahn, T. Tropical rain recycling. Nature 445, 495–496 (2007). https://doi.org/10.1038/445495a
Published:
Issue Date:
DOI: https://doi.org/10.1038/445495a