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Below is the combined list of references from refs_sat.bib and refs_external.bib. It is intended for our group's internal use.

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                1. Brient, F., T. Schneider, Z. Tan, S. Bony, X. Qu, and A. Hall (2015), Shallowness of tropical low clouds as a predictor fo climate models' response to warmingClimate Dynamics, 1–17, doi:10.1007/s00382-015-2846-0.
                2. Chaboureau, J.-P., J.-P. Cammas, J. Duron, P. J. Mascart, N. M. Sitnikov, and H.-J. Voessing (2007), A numerical study of tropical cross-tropopause transport by convective overshootsAtmos. Chem. Phys., 7(7), 1731–1740, doi:10.5194/acp-7-1731-2007.
                3. Chae, J. H., D. L. Wu, W. G. Read, and S. C. Sherwood (2011), The role of tropical deep convective clouds on temperature, water vapor, and dehydration in the tropical tropopause layer (TTL)Atmos. Chem. Phys., 11, 3811–3821, doi:10.5194/acp-11-3811-2011.
                4. Chung, E. S., B. J. Sohn, and V. Ramanathan (2004), Moistening Processes in the Upper Troposphere by Deep Convection: A Case Study over the Tropical Indian OceanJ. Meteorol. Soc. Jpn., 82(3), 959–965.
                5. Chung, E. S., B. J. Sohn, J. Schmetz, and M. Koenig (2007), Diurnal variation of upper tropospheric humidity and its relations to convective activities over tropical AfricaAtmos. Chem. Phys., 7(10), 2489–2502, doi:10.5194/acp-7-2489-2007.
                6. Claud, C., B. Alhammoud, B. M. Funatsu, C. Lebeaupin Brossier, J.-P. Chaboureau, K. Béranger, and P. Drobinski (2012), A high resolution climatology of precipitation and deep convection over the Mediterranean region from operational satellite microwave data: development and application to the evaluation of model uncertaintiesNat. Hazards and Earth Syst. Sci, 12, 785–798, doi:10.5194/nhess-12-785-2012.
                7. Cronin, T. W. and A. A. Wing (2017), Clouds, Circulation, and Climate Sensitivity in a Radiative-Convective Equilibrium Channel ModelJ. Adv. Model. Earth Syst., 9(8), 2883–2905, doi:10.1002/2017MS001111.
                8. Emanuel, K. A., J. D. Neelin, and C. S. Bretherton (1994), On large-scale circulations in convecting atmospheresQ. J. R. Meteorol. Soc., 120(519), 1111–1143, doi:10.1002/qj.49712051902.
                9. Folkins, I., K. K. Kelly, and E. M. Weinstock (2002), A simple explanation for the increase in relative humidity between 11 and 14 km in the tropicsJ. Geophys. Res., 107(D23), 4736, doi:10.1029/2002JD002185.
                10. Folkins, I. and R. V. Martin (2004), The Vertical Structure of Tropical Convection and Its Impact on the Budgets of Water Vapor and OzoneJ. Atmos. Sci., 62, 1560–1573.
                11. Folkins, I., P. Bernath, C. Boone, L. J. Donner, A. Eldering, G. Lesins, R. V. Martin, B.-M. Sinnhuber, and K. Walker (2006), Testing convective parameterizations with tropical measurements of HNO3, CO, H2O, and O3: Implications for the water vapor budgetJ. Geophys. Res., 111, D23304, doi:10.1029/2006JD007325.
                12. Highwood, E. J. and B. J. Hoskins (1998), The tropical tropopauseQ. J. R. Meteorol. Soc., 124(549), 1579–1604, doi:10.1002/qj.49712454911.
                13. Jiang, J. H., H. Su, C. Zhai, S. T. Massie, M. R. Schoeberl, P. R. Colarco, S. Platnick, Y. Gu, and K. N. Liou (2011), Influence of convection and aerosol pollution on ice cloud particle effective radiusAtmos. Chem. Phys., doi:10.5194/acp-11-457-2011.
                14. Kiladis, G. N., K. H. Straub, G. C. Reid, and K. S. Gage (2001), Aspects of interannual and intraseasonal variability of the tropopause and lower stratosphereQ. J. R. Meteorol. Soc., 127(576), 1961–1983, doi:10.1002/qj.49712757606.
                15. Kubar, T. L., D. L. Hartmann, and R. Wood (2007), Radiative and Convective Driving of Tropical High CloudsJ. Climate, 20(22), 5510–5526, doi:10.1175/2007JCLI1628.1.
                16. Mapes, B. E. (2016), Gregarious convection and radiative feedbacks in idealized worldsJ. Adv. Model. Earth Syst., 8(2), 1029–1033, doi:10.1002/2016MS000651.
                17. Rossow, W. B. and C. Pearl (2007), 22-Year survey of tropical convection penetrating into the lower stratosphereGeophys. Res. Lett., 34(4), L04803, doi:10.1029/2006GL028635.
                18. Sherwood, S. C., R. Roca, T. M. Weckwerth, and N. G. Andronova (2010), Tropospheric water vapor, convection, and climateRev. Geophys., 48(2), RG2001, doi:10.1029/2009RG000301.
                19. Sherwood, S. C., S. Bony, and J.-L. Dufresne (2014), Spread in model climate sensivity traced to atmospheric convective mixingNature, 505(7481), 37–42, doi:10.1038/nature12829.
                20. Tobin, I., S. Bony, and R. Roca (2012), Observational Evidence for Relationships between the Degree of Aggregation of Deep Convection, Water Vapor, Surface Fluxes, and RadiationJ. Climate, 25(20), 6885–6904, doi:10.1175/JCLI-D-11-00258.1.
                21. Wing, A. A. and K. A. Emanuel (2014), Physical mechanisms controlling self-aggregation of convection in idealized numerical modeling simulationsJ. Adv. Model. Earth Syst., 6(1), 59–74, doi:10.1002/2013MS000269.
                22. Wu, J., A. D. Del Genio, M.-S. Yao, and A. B. Wolf (2009), WRF and GISS SCM simulations of convective updraft properties during TWP-ICEJ. Geophys. Res., 114, D04206, doi:10.1029/2008JD010851.
                23. Yang, G. Y. and J. Slingo (2000), The Diurnal Cycle in the TropicsMon. Weather Rev., 129, 784–798.