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Allan, R. P., V. Ramaswamy, and A. Slingo (2002), Diagnostic analysis of atmospheric moisture and clear-sky radiative feedback in the Hadley Centre and Geophysical Fluid Dynamics Laboratory GFDL climate models, J. Geophys. Res., 107(D17), doi:10.1029/2001JD001131.
Bony, S., J.-L. Dufresne, H. Le Treut, J.-J. Morcrette, and C. Senior (2004), On dynamic and thermodynamic components of cloud changes, Climate Dynamics, 22(2), 71–86, doi:10.1007/s00382-003-0369-6.
Bony, S., R. Colman, V. M. Kattsov, R. P. Allan, C. S. Bretherton, J.-L. Dufresne, A. Hall, S. Hallegatte, M. M. Holland, W. Ingram, D. A. Randall, B. J. Soden, G. Tselioudis, and M. J. Webb (2006), How Well Do We Understand and Evaluate Climate Change Feedback Processes?, J. Climate, 19, 3445–3482.
Bony, S., B. Stevens, D. Coppin, T. Becker, K. A. Reed, A. Voigt, and B. Medeiros (2016), Thermodynamic control of anvil cloud amount, Proc. Nat. Aca. Sci., doi:10.1073/pnas.1601472113.
Feldl, N. and S. Bordoni (2016), Characterizing the Hadley Circulation Response through Regional Climate Feedbacks, J. Climate, 29(2), 613-622, doi:10.1175/JCLI-D-15-0424.1.
de F. Forster, P. M. and M. Collins (2003), Quantifying the water vapour feedback associated with post-Pinatubo global cooling, Climate Dynamics, 25(2), 207–214.
Hall, A. and S. Manabe (2000), Effect of water vapor feedback on internal and anthropogenic variations of the global hydrologic cycle, J. Geophys. Res., 105(D5), 6935–6944.
Minschwaner, K. and A. E. Dessler (2004), Water Vapor Feedback in the Tropical Upper Troposphere: Model Results and Observations, J. Climate, 17, 1272–1282, doi:10.1175/1520-0442(2004)017<1272:WVFITT>2.0.CO;2.
Noda, A. T., T. Seiki, M. Satoh, and Y. Yamada (2016), High cloud size dependency in the applicability of the fixed anvil temperature hypothesis using global nonhydrostatic simulations, Geophys. Res. Lett., 43(5), 2307–2314, doi:10.1002/2016GL067742.
Philipona, R., B. Duerr, A. Ohmura, and C. Ruckstuhl (2005), Anthropogenic greenhouse forcing and strong water vapor feedback increase temperature in Europe, Geophys. Res. Lett., 32, doi:10.1029/2006GL023624.
Rieck, M., L. Nuijens, and B. Stevens (2012), Marine Boundary Layer Cloud Feedbacks in a Constant Relative Humidity Atmosphere, J. Atmos. Sci., 69(8), 2538–2550, doi:10.1175/JAS-D-11-0203.1.
Slingo, A., J. A. Pamment, R. P. Allan, and P. S. Wilson (2000), Water Vapor Feedbacks in the ECMWF Reanalyses and Hadley Centre Climate Model, J. Climate, 13, 3080–3098.
Soden, B. J., R. T. Wetherald, G. L. Stenchikov, and A. Robock (2002), Global Cooling After the Eruption of Mount Pinatubo: A Test of Climate Feedback by Water Vapor, Science, 296, 727–730.
Soden, B. J. and I. M. Held (2006), An assessment of climate feedbacks in coupled ocean-atmosphere models, J. Climate, 19(14), 3354–3360, doi:10.1175/JCLI3799.1.
Soden, B. J. and R. Fu (1995), A Satellite Analysis of Deep Convection, Upper-Tropospheric Humidity, and the Greenhouse Effect, J. Climate, 8, 2333–2351.
Stainforth, D. A., T. Aina, C. Christensen, M. Collins, N. Faull, D. J. Frame, J. A. Kettleborough, S. Knight, A. Martin, J. M. Murphy, C. Piani, D. Sexton, L. A. Smith, R. A. Spicer, A. J. Thorpe, and M. R. Allen (2005), Uncertainty in predictions of the climate response to rising levels of greenhouse gases, Nature, 433, 403–406.
Stephens, G. L., S. Tsay, P. W. Stackhouse Jr., and P. J. Flatau (1990), The relevance of the microphysical and radiative properties of cirrus clouds to climate and climatic feedback, J. Atmos. Sci., 47(14), 1742–1753, doi:10.1175/1520-0469(1990)047<1742:TROTMA>2.0.CO;2.
Su, H., R. W. Read, J. H. Jiang, J. W. Waters, D. L. Wu, and E. J. Fetzer (2006), Enhanced positive water vapor feedback associated with tropical deep convection: New evidence from Aura MLS, Geophys. Res. Lett., 33, L05709, doi:10.1029/2005GL025505.
Watterson, I. G., M. R. Dix, and R. A. Colman (1999), A comparison of present and doubled CO2 climates and feedbacks simulated by three general circulation models, J. Geophys. Res., 104(D2), 1943–1956.
Zelinka, M. D. and D. L. Hartmann (2010), Why is longwave cloud feedback positive?, J. Geophys. Res.: Atm., 115(D16), D16117, doi:10.1029/2010JD013817,.
Zelinka, M. D. and D. L. Hartmann (2011), The observed sensitivity of high clouds to mean surface temperature anomalies in the tropics, J. Geophys. Res., 116(D23), D23103, doi:10.1029/2011JD016459,.
Zelinka, M. D., S. A. Klein, K. E. Taylor, T. Andrews, M. J. Webb, J. M. Gregory, and P. M. Forster (2013), Contributions of Different Cloud Types to Feedbacks and Rapid Adjustments in CMIP5, J. Climate, 26(14), 5007–5027, doi:10.1175/JCLI-D-12-00555.1.