Upper-tropospheric moistening in response to anthropogenic warming
- aRosenstiel School of Marine and Atmospheric Science, University of Miami, Miami, FL 33149;
- bSchool of Earth and Environmental Sciences, Seoul National University, Seoul 151-747, Korea; and
- cNational Climatic Data Center, National Oceanic and Atmospheric Administration, Asheville, NC 28801
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Edited by John H. Seinfeld, California Institute of Technology, Pasadena, CA, and approved June 27, 2014 (received for review May 23, 2014)
Significance
The fact that water vapor is the most dominant greenhouse gas underscores the need for an accurate understanding of the changes in its distribution over space and time. Although satellite observations have revealed a moistening trend in the upper troposphere, it has been unclear whether the observed moistening is a facet of natural variability or a direct result of human activities. Here, we use a set of coordinated model experiments to confirm that the satellite-observed increase in upper-tropospheric water vapor over the last three decades is primarily attributable to human activities. This attribution has significant implications for climate sciences because it corroborates the presence of the largest positive feedback in the climate system.
Abstract
Water vapor in the upper troposphere strongly regulates the strength of water-vapor feedback, which is the primary process for amplifying the response of the climate system to external radiative forcings. Monitoring changes in upper-tropospheric water vapor and scrutinizing the causes of such changes are therefore of great importance for establishing the credibility of model projections of past and future climates. Here, we use coupled ocean–atmosphere model simulations under different climate-forcing scenarios to investigate satellite-observed changes in global-mean upper-tropospheric water vapor. Our analysis demonstrates that the upper-tropospheric moistening observed over the period 1979–2005 cannot be explained by natural causes and results principally from an anthropogenic warming of the climate. By attributing the observed increase directly to human activities, this study verifies the presence of the largest known feedback mechanism for amplifying anthropogenic climate change.
Footnotes
- ↵1To whom correspondence should be addressed. Email: b.soden{at}miami.edu.
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Author contributions: E.-S.C. and B.S. designed research; E.-S.C. and B.S. performed research; E.-S.C., B.S., B.J.S., and L.S. analyzed data; and E.-S.C., B.S., and B.J.S. wrote the paper.
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The authors declare no conflict of interest.
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This article is a PNAS Direct Submission.
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This article contains supporting information online at www.pnas.org/lookup/suppl/doi:10.1073/pnas.1409659111/-/DCSupplemental.
Freely available online through the PNAS open access option.
