More evidence of a positive WV feedback?
I know I've already asked several questions on the water vapor feedback before, and I've personally found the evidence of a positive WV feedback quite compelling for some time now, but a paper was recently accepted to JGR atmos which effectively rebuts the Paltridge 2009 paper on humidity trends from the NCEP reanalysis:http://www.gerkynet.com/meteo/paltrigde08.pdf
P09 purported to find negative trends in specific humidity above 850 hPa, meaning a negative water vapor feedback. However, in their new paper "Trends in tropospheric humidity from reanalysis systems", Dessler et al. study other, more modern reanalyses, and discuss the many issues with the NCEP reanalysis data. They conclude:
"P09 calculated trends of specific humidity with time over the past few decades in the NCEP/NCAR reanalysis and found that the specific humidity, in particular in the tropical mid and upper troposphere, was decreasing. They concluded that this potentially cast doubt on the general consensus that the global water vapor feedback was strongly positive [e.g., Dessler and Sherwood, 2009]. We have extended the analysis of P09 by addressing two crucial issues, namely whether other reanalyses reproduce this and what time scale of climate fluctuation is associated with the negative water vapor trends. We have analyzed five different reanalyses, including the NCEP/NCAR
reanalysis. Rather than calculate trends with time, as P09 did, we instead regressed atmospheric humidity against surface temperatures for the tropics and mid-latitudes. In response to short time-scale climate variations (e.g., ENSO cycles), there is good agreement among the reanalyses on the connection between atmospheric water vapor and surface temperature: specific humidity increases with increasing surface temperature in the tropical mid and upper troposphere, as well as almost everywhere else. This is in good agreement with both theory and observation.
The picture is different when long-term climate variations are considered. The NCEP/NCAR reanalysis shows decreases in specific humidity in the tropical mid and upper troposphere with increasing tropical surface temperature. Such behavior implies that the water vapor feedback in response to long-term climate fluctuations would be negative, and would therefore have a different sign depending on the time-scale of the climate variation. No theory or model supports this, nor do analyses of long-term water vapor measurements or paleoclimate data.
In addition, the other reanayses, including the newest reanalyses (ERA-interim and MERRA), which were specifically designed to better reproduce long-term trends, do not manifest this behavior. Finally, we pointed out that the NCEP/NCAR reanalysis contains large biases in the tropical mid and upper tropospheric specific humidity, and does not reproduce the moistening of the tropical upper troposphere during the strong 1998 El Nino, further casting doubt on that reanalysis’ water vapor fields in that region.
Based on the available evidence, it is our judgment that negative trends in the tropical mid and upper troposphere in response to long-term climate change are spurious. This is clearly the most parsimonious explanation, and it is in accord with virtually all of the independent lines of evidence (models, observations, theory, newer reanalyses)."
Add this to the studies using satellite data; e.g.
Soden 2005: http://www.gfy.ku.dk/~kaas/forc&feedb2008/Articles/Soden.pdf
Dessler and Zhang 2008: http://www.agu.org/pubs/crossref/2008/2008GL035333.shtml
And it looks like the case for a strong and positive water vapor feedback is becoming harder and harder to deny.
Thoughts? Any other useful references on the topic?
The Dessler 2010 study I quote has been accepted to JGR atmospheres (see http://www.agu.org/journals/jd/papersinpress.shtml#id2010JD014192 ), but has not yet been published, which means that free online copies probably aren't floating around yet. I can email a copy of the preprint upon request.
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David,
Thanks for sticking to peer-reviewed research, but I have several issues with your answer:
1) RH does not need to remain flat for the WV feedback to be positive -- only a positive trend in q is necessary. Paltridge 09 found negative trends in both q and RH, implying a negative WV feedback. BUT, satellite studies of radiance have found that the constant RH assumption used by modelers is not unreasonable. And Dessler 2010 show that P09's data is unreliable.
2) I've read Spencer 2010, and I know that even Spencer is unsure of how the "feedback signal" he found is related to climate sensitivity, concluding
"...even if they do represent feedback operating on intraseasonal to interannual time scales it is not obvious how they relate to long-term climate sensitivity."
Lin 2010, "Can climate sensitivity be estimated from short-term relationships of top-of-atmosphere net radiation and surface temperature?"
Find that Spencer's method does NOT capture the true feedback signal.