Surface global warming has stalled since around 2000 despite increasing atmospheric CO2. A study finds that recent strengthening of Pacific trade winds has enhanced heat transport from the surface to ocean depths, explaining most of the slowed surface warming.
References
Trenberth, K. E. & Fasullo, J. T. Earth's Future 1, 19–32 (2013).
England, M. H. et al. Nature Clim. Change 4, 222–227 10.1038/nclimate2106 (2014).
Kosaka, Y. & Xie, S.-P. Nature 501, 403–407 (2013).
Fyfe, J. C. & Gillett, N. P. Nature Clim. Change 4, 150–151 (2014).
Luo, J.-J., Sasaki, W. & Masumoto, Y. Proc. Natl Acad. Sci. USA 109, 18701–18706 (2012).
Chikamoto, Y., Kimoto, M., Watanabe, M., Ishii, M. & Mochizuki, T. Geophys. Res. Lett. 39, L21710 (2012).
Meehl, G. A. et al. Nature Clim. Change 1, 360–364 (2011).
Watanabe, M. et al. Geophys. Res. Lett. 40, 3175–3179 (2013).
Levitus, S. et al. Geophys. Res. Lett. 39, L10603 (2012).
Balmaseda, M. A., Trenberth, K. E. & Källén, E. Geophys. Res. Lett. 40, 1754–1759 (2013).
Reynolds, R. W., Rayner, N. A., Smith, T. M., Stokes, D. C. & Wang, W. J. Clim. 15, 1609–1625 (2002).
Dee, D. P. et al. Q. J. R. Meteorol. Soc. 137, 553–597 (2011).
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Kosaka, Y. Increasing wind sinks heat. Nature Clim Change 4, 172–173 (2014). https://doi.org/10.1038/nclimate2138
Published:
Issue Date:
DOI: https://doi.org/10.1038/nclimate2138
- Springer Nature Limited
This article is cited by
-
The Performance of Dual-Frequency Polarimetric Scatterometer in Sea Surface Wind Retrieval
Journal of Ocean University of China (2019)