Abstract
Convective processes affect large-scale environments through cloud-radiation interaction, cloud microphysical processes, and surface rainfall processes. Over the last three decades, cloud-resolving models (CRMs) have demonstrated to be capable of simulating convective-radiative responses to an imposed largescale forcing. The CRM-produced cloud and radiative properties have been utilized to study the convective-related processes and their ensemble effects on large-scale circulations. This review summarizes the recent progress on the understanding of convective processes with the use of CRM simulations, including precipitation processes; cloud microphysical and radiative processes; dynamical processes; precipitation efficiency; diurnal variations of tropical oceanic convection; local-scale atmosphere-ocean coupling processes; and tropical convective-radiative equilibrium states. Two different ongoing applications of CRMs to general circulation models (GCMs) are discussed: replacing convection and cloud schemes for studying the interaction between cloud systems and large-scale circulation, and improving the schemes for climate simulations.
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References
Adamec, D., R. L. Elsberry, R. W Garwood, and R. L. Haney, 1981: An embedded mixed-layer-ocean circulation model. Dyn. Atmos. Oceans, 6(2), 69–96.
Braham, R. R. Jr., 1952: The water and energy budgets of the thunderstorm and their relation to thunderstorm development. J. Meteor., 9, 227–242.
Cao, Z., and H. Cho, 1995: Generation of moist vorticity in extratropical cyclones. J. Atmos. Sci., 52, 3263–3281.
Chao, J., 1961: A nonlinear analysis of development of thermal convection in a stratified atmosphere. Acta Meteorologica Sinica, 31, 191–204. (in Chinese)
Chao, J., 1962: On the nonlinear impacts of stratification and wind on development of small-scale disturbances. Acta Meteorologica Sinica, 32, 164–176. (in Chinese)
Chao, W. C., and S. J. Lin, 1994: Tropical intraseasonal oscillation, super cloud clusters, and cumulus convection schemes. J. Atmos. Sci., 51, 1282–1297.
Chou, M.-D., and M. J. Suarez, 1994: An efficient thermal infrared radiation parameterization for use in General Circulation Model. NASA Technical Memorandum 104606, Vol. 3, 85pp.
Chou, M.-D., D. P. Kratz, and W. Ridgway, 1991: IR radiation parameterization in numerical climate studies. J. Climate, 4, 424–437.
Chou, M.-D., M. J. Suarez, C.-H. Ho, M. M.-H. Yan, and K.-T. Lee, 1998: Parameterizations for cloud overlapping and shortwave single-scattering properties for use in General Circulation and Cloud Ensemble Models. J. Climate, 11, 202–214.
Cui, X., and X. Li, 2006: The role of surface evaporation in surface rainfall processes. J. Geophys. Res., 111, D17112, doi:10.1029/2005JD006876.
Cui, X., Y. Zhu, and X. Li, 2007: Cloud microphysical properties in tropical convective and stratiform regions. Meteor. Atmos. Phys., 98, 1–11.
Das, S., D. Johnson and W.-K. Tao, 1999: Single-column and cloud ensemble model simulations of TOGA COARE convective systems. J. Meteor. Soc. Japan, 77, 803–826.
Doswell, C. A., III, H. E. Brooks, and R. A. Maddox, 1996: Flash flood forecasting: An ingredients-based methodology. Wea. Forecasting, 11, 560–581.
Droegemeier, K. K., and S. M. Lazarus, 1993: The influence of helicity on numerically simulated convective storms. Mon. Wea. Rev., 121, 2005–2029.
Emanuel, K. A., 1979: Inertial instability and mesoscale convective systems. Part I: Linear theory of inertial instability in rotating viscous fluids. J. Atmos. Sci., 36, 2425–2449.
Fovell, R. G., and Y. Ogura, 1988: Numerical simulation of a midlatitude squall line in two dimensions. J. Atmos. Sci., 45, 3846–3879.
Gao, S., 2007: A three dimensional dynamic vorticity vector associated with tropical oceanic convection. J. Geophys. Res., 112, doi: 10.1029/2006JD008247.
Gao, S., and X. Li, 2008: Cloud Resolving modeling of Convective Processes. Springer, Netherlands, 272pp.
Gao, S., T. Lei, and Y. Zhou, 2002: Moist potential vorticity anomaly with heat and mass forcings in torrential rain system. Chinese Physical Letters, 19, 878–880.
Gao, S., F. Ping, X. Li, and W.-K. Tao, 2004: A convective vorticity vector associated with tropical convection: A 2D cloud-resolving modeling study. J. Geophys. Res., 109, D14106, doi: 10.1029/2004JD004807.
Gao, S., X. Cui, Y. Zhu, and X. Li, 2005a: Surface rainfall processes as simulated in a cloud resolving model. J. Geophys. Res., 110, D10202, doi: 10.1029/2004JD005467.
Gao, S., X. Cui, Y. Zhou, X. Li, and W.-K. Tao, 2005b: A modeling study of moist and dynamic vorticity vectors associated with 2D tropical convection. J. Geophys. Res., 110, D17104, doi: 10.1029/2004JD005675.
Gao, S., F. Ping, and X. Li, 2006a: Cloud microphysical processes associated with the diurnal variations of tropical convection: A 2D cloud resolving modeling study. Meteor. Atmos. Phys., 91, 9–16.
Gao, S., F. Ping, and X. Li, 2006b: Tropical heat/water vapor quasi-equilibrium and cycle as simulated in a 2D cloud resolving model. Atmospheric Research, 79, 15–29.
Gao, S., F. Ping, X. Cui, and X. Li, 2006c: Short timescale air-sea coupling in the tropical deep convective regime. Meteor. Atmos. Phys., 93, 37–44.
Gao, S., L. Ran, and X. Li, 2006d: Impacts of ice microphysics on rainfall and thermodynamic processes in the tropical deep convective regime: A 2D cloud-resolving modeling study. Mon. Wea. Rev., 134, 3015–3024.
Gao, S., Y. Zhou, and X. Li, 2007a: Effects of diurnal variations on tropical equilibrium states: A two-dimensional cloud-resolving modeling study. J. Atmos. Sci., 64, 656–664.
Gao, S., X. Li, W.-K. Tao, C.-L. Shie, and S. Lang, 2007b: Convective and moist vorticity vectors associated with three-dimensional tropical oceanic convection during KWAJEX. J. Geophys. Res., 112, D01104, doi:10.1029/2006JD007179.
Grabowski, W. W., 1998: Toward cloud resolving modeling of large-scale tropical circulations: A simple cloud microphysics parameterization. J. Atmos. Sci., 55, 3283–3298.
Grabowski, W. W., 2001: Coupling cloud processes with the large-scale dynamics using the cloud-resolving convection parameterization (CRCP). J. Atmos. Sci., 58, 978–997.
Grabowski, W. W., 2003: Impact of ice microphysics on multiscale organization of tropical convection in two-dimensional cloud-resolving simulations. Quart. J. Roy. Meteor. Soc., 129, 67–81.
Grabowski, W. W., and P. K. Smolarkiewicz, 1999: CRCP: A cloud-resolving convection parameterization for modeling the tropical convecting atmosphere. Physica D, 133, 171–178.
Grabowski, W. W., M. W. Moncrieff, and J. T. Kiehl, 1996a: Long-term behavior of precipitating tropical cloud systems: A numerical study. Quart. J. Roy. Meteor. Soc., 122, 1019–1042.
Grabowski, W. W., X. Wu, and M. W. Moncrieff, 1996b: Cloud-resolving model of tropical cloud systems during Phase III of GATE. Part I: Two-dimensional experiments. J. Atmos. Sci., 53, 3684–3709.
Grabowski, W. W., X. Wu, M. W. Moncrieff, and W. D. Hall, 1998: Cloud-resolving model of tropical cloud systems during Phase III of GATE. Part II: Effects of resolution and the third spatial dimension. J. Atmos. Sci., 55, 3264–3282.
Grabowski, W. W., X. Wu, and M. W. Moncrieff, 1999: Cloud-resolving model of tropical cloud systems during Phase III of GATE. Part III: Effects of cloud microphysics. J. Atmos. Sci., 56, 2384–2402.
Grabowski, W. W., J.-I. Yano, and M. W. Moncrieff, 2000: Cloud resolving modeling of tropical circulations driven by large-scale SST gradients. J. Atmos. Sci., 57, 2022–2039.
Grabowski, W. W., and M. W. Moncrieff, 2001: Largescale organization of tropical convection in two-dimensional explicit numerical simulations. Quart. J. Roy. Meteor. Soc., 127, 445–468.
Gray, W. M., and R. W. Jacobson, 1977: Diurnal variation of deep cumulus convection. Mon. Wea. Rev., 105, 1171–1188.
Heymsfield, G. M., and S. Schotz, 1985: Structure and evolution of a severe squall line over Oklahoma. Mon. Wea. Rev., 113, 1563–1589.
Johnson, D. E., W.-K. Tao, J. Simpson, and C.-H. Sui, 2002: A study of the response of deep tropical clouds to large-scale thermodynamic forcings. Part I: Modeling strategies and simulations of TOGA COARE convective systems. J. Atmos. Sci., 59, 3492–3518.
Khairoutdinov, M., and D. A. Randall, 2001: A cloud resolving model as a cloud parameterization in the NCAR Community Climate Model: Preliminary results. Geophys. Res. Lett., 28, 3617–3620.
Khairoutdinov, M., D. A. Randall, and C. DeMott, 2005: Simulations of the atmospheric general circulations using a cloud-resolving model as a superparameterization of physical processes. J. Atmos. Sci., 62, 2136–2154.
Klemp, J. B., and R. B. Wilhelmson, 1978: The simulation of three-dimensional convective storm dynamics. J. Atmos. Sci., 35, 1070–1093.
Kraus, E. B., 1963: The diurnal precipitation change over the sea. J. Atmos. Sci., 20, 546–551.
Krueger, S. K., 1988: Numerical simulation of tropical cumulus clouds and their interaction with the subcloud layer. J. Atmos. Sci., 45, 2221–2250.
Krueger, S. K., Q. Fu, K. N. Liou, and H.-N. S. Chin, 1995: Improvement of an ice-phase microphysics parameterization for use in numerical simulations of tropical convection. J. Appl. Meteor., 34, 281–287.
Lang, S., W.-K. Tao, J. Simpson, and B. Ferrier, 2003: Modeling of convective-stratiform precipitation processes: Sensitivity to partitioning methods. J. Appl. Meteor., 42, 505–527.
Lau, K.-M., L. Peng, C.-H. Sui, and T. Nakazawa, 1989: Super cloud clusters, westerly wind bursts, 30–60 day oscillations, and ENSO: A unified view. J. Meteor. Soc. Japan, 67, 205–219.
Lau, K.-M., T. Nakazawa, and C.-H. Sui, 1991: Observations of cloud cluster hierarchy over the tropical western Pacific. J. Geophys. Res., 96, 3197–3208.
Lau, K.-M., C.-H. Sui, and W.-K. Tao, 1993: A preliminary study of the tropical water cycle using the Goddard Cumulus Ensemble model. Bull. Amer. Meteor. Soc., 74, 1313–1321.
Lau, K.-M., C.-H. Sui, M.-D. Chou, and W.-K. Tao, 1994: An inquiry into the cirrus-cloud thermostat effect for tropical sea surface temperature. Geophys. Res. Lett., 21, 1157–1160.
Li, X., 2004: Cloud modeling in the tropical deep convective regime. Observation, Theory, and Modeling of Atmospheric Variability, X. Zhu, Ed., World Sci., River Edge, N. J., 206–223.
Li, X., 2006: Cloud microphysical and precipitation responses to a large-scale forcing in the tropical deep convective regime. Meteor. Atmos. Phys., 94, 87–102.
Li, X., C.-H. Sui, D. Adamec, and K.-M. Lau, 1998: Impacts of precipitation in the upper ocean in the western Pacific warm pool during TOGA COARE. J. Geophys. Res., 103, 5347–5359.
Li, X., C.-H. Sui, K.-M. Lau, and M.-D. Chou, 1999: Large-scale forcing and cloud-radiation interaction in the tropical deep convective regime. J. Atmos. Sci., 56, 3028–3042.
Li, X., C.-H. Sui, K.-M. Lau, and D. Adamec, 2000: Effects of precipitation on ocean mixed-layer temperature and salinity as simulated in a 2-D coupled ocean-cloud resolving atmosphere model. J. Meteor. Soc. Japan, 78, 647–659.
Li, X., C.-H. Sui, and K.-M. Lau, 2002a: Precipitation efficiency in the tropical deep convective regime: A 2D cloud resolving modeling study. J. Meteor. Soc. Japan, 80, 205–212.
Li, X., C.-H. Sui, and K.-M. Lau, 2002b: Interactions between tropical convection and its environment: An energetics analysis of a 2-D cloud resolving simulation. J. Atmos. Sci., 59, 1712–1722.
Li, X., C.-H. Sui, K.-M. Lau, and W.-K. Tao, 2005: Tropical convective responses to microphysical and radiative processes: A 2D cloud-resolving modeling study. Meteor. Atmos. Phys., 90, 245–259.
Li, X., S. Zhang, and D.-L. Zhang, 2006: Thermodynamic, cloud microphysics and rainfall responses to initial moisture perturbations in the tropical deep convective regime. J. Geophys. Res., 111, D14207, doi:10.1029/2005JD006968.
Liang, X.-Z., and X. Wu, 2005: Evaluation of a GCM subgrid cloud-radiation interaction parameterization using cloud-resolving model simulations. Geophys. Res. Lett., 32, L06801, doi:10.1029/2004GL022301.
Lilly, D. K., 1986: The structure, energetics and propagation of rotating convective storms. Part II: Helicity and storm stabilization. J. Atmos. Sci., 43, 126–140.
Lipps, F. B., and R. S. Hemler, 1986: Numerical simulation of deep tropical convection associated with large-scale convergence. J. Atmos. Sci., 43, 1796–1816.
Lin, Y. L., R. D. Farley, and H. D. Orville, 1983: Bulk parameterization of the snow field in a cloud model. J. Climate Appl. Meteor., 22, 1065–1092.
Liu, C., and M. W. Moncrieff, 1998: A numerical study of the diurnal cycle of tropical oceanic convection. J. Atmos. Sci., 55, 2329–2344.
Louis, J. F., M. Tiedke, and J. F. Geleyn, 1982: A short history of the PBL parameterization at ECMWF. Workshop on Planetary Boundary Layer Parameterization, ECMWF. Reading, UK, 59–80.
McCumber, M., W.-K. Tao, J. Simpson, R. Penc, and S.-T. Soong, 1991: Comparison of ice-phase microphysical parameterization schemes using numerical simulations of tropical convection. J. Appl. Meteor., 30, 985–1004.
Moncrieff, M. W., and M. J. Miller, 1976: The dynamics and simulation of tropical cumulonimbus and squall line. Quart. J. Roy. Meteor. Soc., 102, 373–394.
Moncrieff, M. W., and W.-K. Tao, 1999: Cloud-resolving models. Global Water and Energy Cycles, K. Browning and R. J. Gurney, Eds., Cambridge University Press, 200–209.
Nakajima, K., and T. Matsuno, 1988: Numerical experiments concerning the origin of cloud clusters in the tropical atmosphere. J. Meteor. Soc. Japan, 66, 309–329.
Nakajima, T., M. Tsukamoto, Y. Tsushima, A. Numaguti, and T. Kimura, 2000: Modeling of the radiative process in an atmospheric general circulation model. Appl. Opt., 39, 4869–4878.
Nakazawa, T., 1988: Tropical super clusters within intraseasonal variations over the western Pacific. J. Meteor Soc. Japan, 66, 823–839.
Nicholls, M. E., 1987: A comparison of the results of a two-dimensional numerical simulation of a tropical squall line with observations. Mon. Wea. Rev., 115, 3055–3077.
Niiler, P. P., and E. B. Kraus, 1977: One-dimensional models. Modeling and Prediction of the Upper Layers of the Ocean, E. B. Kraus, Ed., Pergamon, New York, 143–172.
Numaguti, A., and Y.-Y. Hayashi, 1991: Behavior of cumulus activity and the structures of circulations in an “aqua planet” model. Part I. The structure of the super cloud clusters. J. Meteor. Soc. Japan, 69, 541–561.
Peng, L., C.-H. Sui, K.-M. Lau, and W.-K. Tao, 2001: Genesis and evolution of hierarchical cloud clusters in a two-dimensional cumulus-resolving model. J. Atmos. Sci., 58, 877–895.
Ping, F., Z. Luo, and X. Li, 2008: Kinematics, cloud microphysics, and spatial structures of tropical cloud clusters: A two-dimensional cloud-resolving modeling study. Atmospheric Research, doi: 10.1016/j.atmosres.2007.11.027.
Ping, F., Z. Luo, and X. Li, 2007: Microphysical and radiative effects of ice clouds on tropical equilibrium states: A two-dimensional cloud-resolving modeling study. Mon. Wea. Rev., 135, 2794–2802.
Randall, D. A., Harshvardhan, and D. A. Dazlich, 1991: Diurnal variability of the hydrologic cycle in a general circulation model. J. Atmos. Sci., 48, 40–62.
Randall, D. A., M. Khairoutdinov, A. Arakawa, W. W. Grabowski, 2003: Breaking the cloud parameterization deadlock. Bull. Amer. Meteor. Soc., 84, 1547–1564.
Rotunno, R., J. B. Klemp, and M. L. Weisman, 1988: A theory for strong, long-lived squall lines. J. Atmos. Sci., 45, 463–485.
Rutledge, S. A., and R. V. Hobbs, 1983: The mesoscale and microscale structure and organization of clouds and precipitation in midlatitude cyclones. Part VIII: A model for the “seeder-feeder” process in warmfrontal rainbands. J. Atmos. Sci., 40, 1185–1206.
Rutledge, S. A., and R. V. Hobbs, 1984: The mesoscale and microscale structure and organization of clouds and precipitation in midlatitude cyclones. Part XII: A diagnostic modeling study of precipitation development in narrow cold-frontal rainbands. J. Atmos. Sci., 41, 2949–2972.
Satoh, M., H. Tomita, H. Miura, S. Iga, and T. Nasumo, 2005: Development of a global resolving model—A multi-scale structure of tropical convections. J. Earth Sim., 3, 1–9.
Shie, C.-L, W.-K. Tao, J. Simpson, and C.-H. Sui, 2003: Quasi-equilibrium states in the tropics simulated by a cloud-resolving model. Part I: Specific features and budget analysis. J. Climate, 16, 817–833.
Song, X., X. Wu, G. J. Zhang, and R. Arritt, 2007: Dynamical effects of convective momentum transports on global climate simulations. J. Climate, 64, 4506–4513.
Sui, C.-H., and K.-M. Lau, 1992: Multi-scale phenomena in the tropical atmosphere over the western Pacific. Mon Wea. Rev., 120, 407–430.
Sui, C.-H., and X. Li, 2005: A tendency of cloud ratio associated with the development of tropical water and ice clouds. Terr. Atmos. Oceanic Sci., 16, 419–434.
Sui, C.-H., K.-M. Lau, W.-K. Tao, and J. Simpson, 1994: The tropical water and energy cycles in a cumulus ensemble model. Part I: Equilibrium climate. J. Atmos. Sci., 51, 711–728.
Sui, C.-H., K.-M. Lau, Y. Takayabu, and D. Short, 1997: Diurnal variations in tropical oceanic cumulus ensemble during TOGA COARE. J. Atmos. Sci., 54, 639–655.
Sui, C.-H., X. Li, and K.-M. Lau, 1998: Radiativeconvective processes in simulated diurnal variations of tropical oceanic convection. J. Atmos. Sci., 55, 2345–2359.
Sui, C.-H., X. Li, M.-J. Yang, and H.-L. Huang, 2005: Estimation of Oceanic Precipitation Efficiency in Cloud Models. J. Atmos. Sci., 62, 4358–4370.
Sui, C.-H., X. Li, K.-M. Lau, W.-K. Tao, M.-D. Chou, and M.-J. Yang, 2007a: Convective-radiative-mixing processes in the Tropical Ocean-Atmosphere. Recent Progress in Atmospheric Sciences with Applications to the Asia-Pacific Region, World Scientific Publication. (in press)
Sui, C.-H., X. Li, and M.-J. Yang, 2007b: On the definition of precipitation efficiency. J. Atmos. Sci., 64, 4506–4513.
Tao, W.-K., 2003: Goddard Cumulus Ensemble (GCE) model: Application for understanding precipitation processes. Meteor. Monogr.-Cloud Systems, Hurricanes and TRMM, 29, 107–138.
Tao, W.-K., 2007: Cloud resolving modeling. J. Meteor. Soc. Japan, 85, 305–330.
Tao, W.-K., and J. Simpson, 1984: Cloud interactions and merging: Numerical simulations. J. Atmos. Sci., 41, 2901–2917.
Tao, W.-K., and S.-T. Soong, 1986: The study of the response of deep tropical clouds to mesoscale processes: Three-dimensional numerical experiments. J. Atmos. Sci., 43, 2653–2676.
Tao, W.-K., and J. Simpson, 1989a: Modeling study of a tropical squall-type convective line. J. Atmos. Sci., 46, 177–202.
Tao, W.-K., and J. Simpson, 1989b: A further study of cumulus interaction and mergers: Three-dimensional simulations with trajectory analyses. J. Atmos. Sci., 46, 2974–3004.
Tao, W.-K., and J. Simpson, 1993: The Goddard Cumulus Ensemble model. Part I: Model description. Terrestrial, Atmospheric Oceanic Sciences, 4, 35–72.
Tao, W.-K., and M. Moncrieff, 2003: Cloud Modeling. Encyclopedia of Atmospheric Sciences, Holtin et al., Eds., 539–548.
Tao, W.-K., J. Simpson, and S.-T. Soong, 1987: Statistical properties of a cloud ensemble: A numerical study. J. Atmos. Sci., 44, 3175–3187.
Tao, W.-K., J. Simpson, and M. McCumber, 1989: An ice-water saturation adjustment. Mon. Wea. Rev., 117, 231–235.
Tao, W.-K., J. Simpson, and S.-T. Soong, 1991: Numerical simulation of a subtropical squall line over the Taiwan Strait. Mon. Wea. Rev., 119, 2699–2723.
Tao, W.-K., S. Lang, J. Simpson, C.-H. Sui, B. S. Ferrier, and M.-D. Chou, 1996: Mechanisms of cloud-radiation interaction in the Tropics and midlatitude. J. Atmos. Sci., 53, 2624–2651.
Tao, W.-K., J. Simpson, C.-H. Sui, C.-L. Shie, B. Zhou, K.-M. Lau, and M. W. Moncrieff, 1999: Equilibrium states simulated by cloud-resolving models. J. Atmos. Sci., 56, 3128–3139.
Tao, W.-K., D. Johnson, C.-L. Shie, and J. Simpson, 2004: The atmospheric energy budget and large-scale precipitation efficiency of convective systems during TOGA COARE, GATE, SCSMEX, and ARM: Cloud-resolving model simulations. J. Atmos. Sci., 61, 2405–2423.
Tomita, H., H. Miura, S. Iga, T. Nasuno, and M. Satoh, 2005: A global cloud-resolving simulation: Preliminary results from an aqua planetary experiment. Geophys. Res. Lett., 32, L08805, doi: 10.1029/2005GL022459.
Tompkins, A. M., 2000: The impact of dimensionality on long-term cloud resolving model simulations. Mon. Wea. Rev., 128, 1521–1535.
Tompkins, A. M., and G. C. Craig, 1998: Radiativeconvective equilibrium in a three-dimensional cloud ensemble model. Quart. J. Roy. Meteor. Soc., 124, 2073–2097.
Wang, Y., W.-K. Tao, and J. Simpson, 1996: The impact of ocean surface fluxes on a TOGA COARE convective System. Mon. Wea. Rev., 124, 2100–2125.
Wang, Y., W.-K. Tao, J. Simpson, and S. Lang, 2003: The sensitivity of tropical squall lines (GATE and TOGA COARE) to surface fluxes: 3-D Cloud resolving model simulations, Quart J. Roy. Meteor. Soc., 129, 987–1007.
Wu, X., 2002: Effects of ice microphysics on tropical radiative-convective-oceanic quasi-equilibrium states. J. Atmos. Sci., 59, 1885–1897.
Wu, X., and M. W. Moncrieff, 1996: Collective effects of organized convection and their approximation in general circulation models. J. Atmos. Sci., 53, 1477–1495.
Wu, X., and M. A. LeMone, 1999: Fine structure of cloud patterns within the intraseasonal oscillation during TOGA COARE. Mon. Wea. Rev., 127, 2503–2513.
Wu, X., and M. W. Moncrieff, 1999: Effects of sea surface temperature and large-scale dynamics on the thermodynamic equilibrium state and convection over the tropical western Pacific. J. Geophys. Res., 104, 6093–6100
Wu, X., and M. W. Moncrieff, 2001a: Long-term behavior of cloud systems in TOGA COARE and their interactions with radiative and surface processes. Part III: Effects on the energy budget and SST. J. Atmos. Sci., 58, 1155–1168.
Wu, X., and M.W. Moncrieff, 2001b: Sensitivity of singlecolumn model solutions to convective parameterizations and initial conditions. J. Climate, 14, 2563–2582.
Wu, X., and X.-Z. Liang, 2005a: Radiative effects of cloud horizontal inhomogeneity and vertical overlap identified from a month-long cloud-resolving simulation. J. Atmos. Sci., 62, 4105–4112.
Wu, X., and X. Liang, 2005b: Effect of subgrid cloud-radiation interaction on climate simulations. Geophys. Res. Lett., 32, L24806, doi:10.1029/2005GL024432.
Wu, X., and S. Guimond, 2006: Two-and three-dimensional cloud-resolving model simulations of the mesoscale enhancement of surface heat fluxes by precipitating deep convection. J. Climate, 19, 139–149.
Wu, X., W. W. Grabowski, and M. W. Moncrieff, 1998: Long-term evolution of cloud systems in TOGA COARE and their interactions with radiative and surface processes. Part I: Two-dimensional cloud-resolving model. J. Atmos. Sci., 55, 2693–2714.
Wu, X., W. D. Hall, W. W. Grabowski, M. W. Moncrieff, W. D. Collins, and J. T. Kiehl, 1999: Longterm evolution of cloud systems in TOGA COARE and their interactions with radiative and surface processes. Part II: Effects of ice microphysics on cloud-radiation interaction. J. Atmos. Sci., 56, 3177–3195.
Wu, X., X.-Z. Liang, and G.-J. Zhang 2003: Seasonal migration of ITCZ precipitation across the equator: Why can’t GCMs simulate it? Geophys. Res. Lett., 30(15), 1824, doi:10.1029/2003GL017198.
Wu, X., X.-Z. Liang, and S. Park, 2007a: Cloud-resolving model simulations over the ARM SGP. Mon. Wea. Rev., 135, 2841–2853.
Wu, X., L. Deng, X. Song, and G.-J. Zhang, 2007b: Coupling of convective momentum transport with convective heating in global climate simulations. J. Atmos. Sci., 64, 1334–1349.
Wu, X., L. Deng, X. Song, G. Vettoretti, W. R. Peltier, and G. J. Zhang, 2007c: Impact of a modified convective scheme on the MJO and ENSO in a coupled climate model. Geophys. Res. Lett., 34, L16823, doi:10.1029/2007GL030637.
Xu, K.-M., and D. A. Randall, 1995: Impact of interactive radiative transfer on the macroscopic behavior of cumulus ensembles. Part II: Mechanisms for cloud-radiation interactions. J. Atmos. Sci., 52, 800–817.
Xu, K.-M., and D. A. Randall, 1996: Explicit simulation of cumulus ensembles with the GATE Phase III data: Comparison with observations. J. Atmos. Sci., 53, 3710–3736.
Yano, J.-I., J. C. McWilliams, M. W. Moncrieff, and K. A. Emanuel, 1995: Hierarchical tropical cloud systems in an analog shallow-water model. J. Atmos. Sci., 52, 1723–1742.
Yoshizaki, M., 1986: Numerical simulations of tropical squall-line clusters: Two-dimensional model. J. Meteor. Soc. Japan, 64, 469–491.
Zhang, G.-J., and X. Wu, 2003: Convective momentum transport and perturbation pressure field from a cloud-resolving model simulation. J. Atmos. Sci., 60, 1120–1139.
Zhou, Y., X. Cui, and X. Li, 2006: Contribution of cloud condensate to surface rainfau process. Progress in Natual Science, 16(9), 967–973.
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Wu, X., Li, X. A review of cloud-resolving model studies of convective processes. Adv. Atmos. Sci. 25, 202–212 (2008). https://doi.org/10.1007/s00376-008-0202-6
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DOI: https://doi.org/10.1007/s00376-008-0202-6