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Bretherton, C. S. and A. H. Sobel (2002), A Simple Model of a Convectively Coupled Walker Circulation Using the Weak Temperature Gradient Approximation, J. Climate, 15(20), 2907–2920, doi:10.1175/1520-0442(2002)015<2907:ASMOAC>2.0.CO;2.
Colman, R. A. and B. J. McAvaney (1997), A study of general circulation model climate feedbacks determined from perturbed seasurface temperature experiments, J. Geophys. Res., 102(D16), 19383–19402, doi:10.1029/97JD00206.
Nilsson, J. and K. A. Emanuel (1999), Equilibrium atmospheres of a two-column radiative-convective model, Q. J. R. Meteorol. Soc., 125(558), 2239–2264, doi:10.1002/qj.49712555814.
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.
Rädel, G., T. Mauritsen, B. Stevens, D. Dommenget, D. Matei, K. Bellomo, and A. Clement (2016), Amplification of El Niño by cloud longwave coupling to atmospheric circulation, Nature Geosci., 9(2), 106–110, doi:10.1038/NGEO2630.
Schulz, F. M., K. Stamnes, and F. Weng (1999), VDISORT: An improved and generalized discrete ordinate method for polarized (vector) radiative transfer, J. Quant. Spectrosc. Radiat. Transfer, 61(1), 105–122.
Spurr, R. J. D. (2006), VLIDORT: A linearized pseudo-spherical vector discrete ordinate radiative transfer code for forward model and retrieval studies in multilayer multiple scattering media, J. Quant. Spectrosc. Radiat. Transfer, 102(2), 316–342, doi:10.1016/j.jqsrt.2006.05.005.
Wing, A. A. and K. A. Emanuel (2014), Physical mechanisms controlling self-aggregation of convection in idealized numerical modeling simulations, J. Adv. Model. Earth Syst., 6(1), 59–74, doi:10.1002/2013MS000269.