[1] Mintz Y, Arakawa A. Northern ecosystem initiative climate change bibliography. Technical Report about Moscow Related Studies, 1965, 3:60-66

[2] Manabe S. Simulated climatology of a general circulation model with a hydrologic cycle. Mon. Wea. Rev., 1965, 93: 769-798

[3] Ooyama K. A dynamical model for the study of tropical cyclone development. Geofis. Intern.,1964, 4:187-198

[4] Kuo HL. On formation and intensification of tropical cyclones through latent heat release by cumulus convection. J. Atmos. Sci.,1965, 22:40-63

[5] Kuo HL. Further studies of the parameterization of the influence of cumulus convection on large-scale flow. J. Atmos. Sci., 1974,31: 1232-1240

[6] Arakawa A, W H Schubert. Interactionof a cumulus cloud ensemble with the large-scale environment. Part I. J. Atmos. Sci., 1974,31: 674-701

[7] Gregory D,P R R Rowntree.A mass flux convection scheme with representation of cloud ensemble characteristics and stability dependent closure.Mon. Wea. Rev., 1990, 118: 1483-1506

[8] Gregory D, MJ Miller.A numerical studyof the parameterizationof deep tropical convection. Quart. J. Roy. Meteor. Soc., 1989, 115:1209-1241

[9] Albrecht B A, V Ramanathan, B A Boville. The effects of cumulus moisture transports on the simulation of climate with a general circulation model. J. Atmos. Sci., 1986, 43: 2443-2462

[10] Bougeault Ph. A simple parameterization of the large-scale effects of cumulus convection. Mon. Wea. Rev.,1985, 113: 2108-2121

[11] Tiedtke M. A comprehensive mass flux scheme for cumulus parameterization in large-scale models. Mon. Wea. Rev., 1989,117: 1779-1800