How can Richard Lindzen continue to defend his IRIS hypothesis when the water vapor feedback is positive?
According to the IRIS hypothesis, precipitation efficiency during deep convection events will increase as the planet warms. This, in turn, will significantly reduce water vapor content in the upper troposphere. High cirrus cloud cover will then decrease, leading to an increase in ORL.
In a recent paper, Richard Lindzen made the following claim in support of the IRIS hypothesis:
“Lindzen and Choi [2009] studied variations in the outgoing radiative fluxes with respect to changes in the average tropical temperature in intraseasonal scales. A total negative feedback was deduced from the outgoing long- wave response of the tropics. If a strong positive water vapor feedback is realistic [e.g., Dessler et al., 2008], then the combined effect of water vapor feedback and lapse rate feedback must be more than compensated by a strong unknown process acting on modifying the longwave flux. This process cannot be distinguished from the bulk of the longwave response in the analysis by Lindzen and Choi [2009], but it most likely resides in the combined behavior of clouds and water vapor in the tropics. This leaves open the possibility that a negative feedback such as the iris is operating in the present climate.”
http://www.dgf.uchile.cl/~ronda/Geologia/ronandlin10a.pdf
To me, it seems that the IRIS hypothesis cannot be correct. Dessler (2008) concluded that, “At all altitudes...global-average specific humidity was higher during the warmer periods, with the difference growing with altitude.”
http://geotest.tamu.edu/userfiles/216/Dessler2008b.pdf
However, as mentioned previously, the IRIS hypothesis predicted that tropospheric water vapor content would actually decrease.
How can Lindzen continue to defend his IRIS hypothesis when he also supports Dessler's conclusions?
I forgot to mention this important detail:
In the study quoted above, Lindzen actually assumed that relative humidity would remain constant as the planet warms, which results in a positive water vapor feedback.