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An observationally based constraint on the water-vapor feedback

ScholarsArchive at Oregon State University

Field Value
Title An observationally based constraint on the water-vapor feedback
Names Gordon, N. D. (creator)
Jonko, A. K. (creator)
Forster, P. M. (creator)
Shell, K. M. (creator)
Date Issued 2013-11-22 (iso8601)
Note This is the publisher’s final pdf. The published article is copyrighted by the author(s) and published by John Wiley & Sons Ltd. on behalf of the American Geophysical Union. The published article can be found at: http://onlinelibrary.wiley.com/journal/10.1002/(ISSN)2169-8996.
Abstract The increase in atmospheric concentrations of water vapor with global warming is a
large positive feedback in the climate system. Thus, even relatively small errors in its
magnitude can lead to large uncertainties in predicting climate response to anthropogenic
forcing. This study incorporates observed variability of water vapor over 2002–2009
from the Atmospheric Infrared Sounder instrument into a radiative transfer scheme to
provide constraints on this feedback. We derive a short-term water vapor feedback of
2.2 ± 0.4 Wm⁻²K⁻¹. Based on the relationship between feedback derived over short and
long timescales in twentieth century simulations of 14 climate models, we estimate a
range of likely values for the long-term twentieth century water vapor feedback of
1.9 to 2.8 Wm⁻²K⁻¹. We use the twentieth century simulations to determine the record
length necessary for the short-term feedback to approach the long-term value. In most of
the climate models we analyze, the short-term feedback converges to within 15% of its
long-term value after 25 years, implying that a longer observational record is necessary to
accurately estimate the water vapor feedback.
Genre Article
Access Condition http://creativecommons.org/licenses/by-nc-nd/3.0/us/
Topic water vapor
Identifier Gordon, N. D., A. K. Jonko, P. M. Forster, and K. M. Shell (2013), An observationally based constraint on the water-vapor feedback, Journal of Geophysical Research: Atmospheres, 118, 12,435–12,443. doi:10.1002/2013JD020184.

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