Cloud Resolving Modeling of Tropical Cloud Systems during Phase III of GATE. Part III: Effects of Cloud Microphysics

Abstract Large-scale conditions during the 7-day period of Phase III of the Global Atmospheric Research Program Atlantic Tropical Experiment are used to study effects of cloud microphysics on the convecting tropical atmosphere. Two-dimensional numerical experiments evaluate the effects of extreme changes to the cloud microphysics in the cloud resolving model. The main conclusions are the following. (a) Extreme changes in cloud microphysics affect the temperature and moisture profiles in a way that approximately retains relative humidity profiles in all experiments. (b) With prescribed radiative tendencies, effects of cloud microphysics on surface processes are paramount. Extreme changes in warm rain microphysics indirectly affect the temperature and moisture profiles by modifying surface sensible and latent heat fluxes. For instance, smaller raindrops, and to a lesser degree slower conversion of cloud water into rain, result in enhanced updraft and downdraft cloud mass fluxes, a colder and drier boundary ...

[1]  H. D. Orville,et al.  Bulk Parameterization of the Snow Field in a Cloud Model , 1983 .

[2]  David A. Randall,et al.  Explicit Simulation of Cumulus Ensembles with the GATE Phase III Data: Comparison with Observations , 1996 .

[3]  K. Emanuel,et al.  Moist Convective Scaling: Some Inferences from Three-Dimensional Cloud Ensemble Simulations , 1996 .

[4]  Y. Ogura,et al.  Response of Tradewind Cumuli to Large-Scale Processes , 1980 .

[5]  Q. Fu,et al.  Interactions of Radiation and Convection in Simulated Tropical Cloud Clusters , 1995 .

[6]  Joanne Simpson,et al.  A Double-Moment Multiple-Phase Four-Class Bulk Ice Scheme. Part II: Simulations of Convective Storms in Different Large-Scale Environments and Comparisons with other Bulk Parameterizations , 1995 .

[7]  W. Grabowski Toward Cloud Resolving Modeling of Large-Scale Tropical Circulations: A Simple Cloud Microphysics Parameterization , 1998 .

[8]  J. Kiehl,et al.  Long-term behaviour of precipitating tropical cloud systems: A numerical study , 1996 .

[9]  M. Lemone,et al.  Cumulonimbus vertical velocity events in GATE. Part I: Diameter, intensity and mass flux , 1980 .

[10]  Francis W. Murray,et al.  Ice-Bearing Cumulus Cloud Evolution: Numerical Simulation and General Comparison Against Observations. , 1976 .

[11]  James J. Hack,et al.  The simulated Earth radiation budget of the National Center for Atmospheric Research community climate model CCM2 and comparisons with the Earth Radiation Budget Experiment (ERBE) , 1994 .

[12]  William D. Hall,et al.  Source code documentation for the Clark-Hall cloud-scale model code version g3ch01. Technical note , 1996 .

[13]  D. Gregory,et al.  A numerical study of the parametrization of deep tropical convection , 1989 .

[14]  K. Emanuel,et al.  Moist Convective Velocity and Buoyancy Scales , 1996 .

[15]  Wei-Kuo Tao,et al.  A Study of the Response of Deep Tropical Clouds to Mesoscale Processes: Three-Dimensional Numerical Experiments , 1986 .

[16]  Andrew P. Ingersoll,et al.  Natural Convection as a Heat Engine: A Theory for CAPE , 1996 .

[17]  R. J. Reed,et al.  Structure and Properties of Synoptic-Scale Wave Disturbances in the Intertropical Convergence Zone of the Eastern Atlantic. , 1979 .

[18]  Q. Fu,et al.  Improvements of an ice-phase microphysics parameterization for use in numerical simulations of tropical convection , 1995 .

[19]  S. K. Cox,et al.  Estimates of Radiative Divergence during Phase III of the GARP Atlantic Tropical Experiment Part I. Methodology , 1979 .

[20]  R. Hemler,et al.  Numerical simulation of deep tropical convection associated with large-scale convergence , 1986 .

[21]  C. Sui,et al.  Mechanisms of Cloud-radiation interaction in the tropics and midlatitudes , 1996 .

[22]  S. K. Cox,et al.  Estimates of Radiative Divergence during Phase III of the GARP Atlantic Tropical Experiment: Part II. Analysis of Phase III Results , 1979 .

[23]  Joanne Simpson,et al.  MODELS OF PRECIPITATING CUMULUS TOWERS , 1969 .

[24]  Terry L. Clark,et al.  Numerical simulations with a three-dimensional cloud model: Lateral boundary condition experiments and multicellular severe storm simulations , 1979 .

[25]  E. Kessler On the distribution and continuity of water substance in atmospheric circulations , 1969 .

[26]  Edward J. Zipser,et al.  Cumulonimbus Vertical Velocity Events in GATE. Part II: Synthesis and Model Core Structure , 1980 .

[27]  S. Rutledge,et al.  The Mesoscale and Microscale Structure and Organization of Clouds and Precipitation in Midlatitude Cyclones. VIII: A Model for the “Seeder-Feeder” Process in Warm-Frontal Rainbands , 1983 .

[28]  W. Tao,et al.  Response of Deep Tropical Cumulus Clouds to Mesoscale Processes , 1980 .

[29]  Joanne Simpson,et al.  Comparison of Ice-Phase Microphysical Parameterization Schemes Using Numerical Simulations of Tropical Convection , 1991 .

[30]  Steven K. Krueger,et al.  Numerical simulation of tropical cumulus clouds and their interaction with the subcloud layer , 1988 .

[31]  J. Marshall,et al.  THE DISTRIBUTION OF RAINDROPS WITH SIZE , 1948 .

[32]  R. Houze Observed structure of mesoscale convective systems and implications for large-scale heating , 1989 .

[33]  Wojciech W. Grabowski,et al.  Cloud-Resolving Modeling of Tropical Cloud Systems during Phase III of GATE. Part I: Two-Dimensional Experiments. , 1996 .

[34]  A. Arakawa,et al.  The Macroscopic Behavior of Cumulus Ensembles Simulated by a Cumulus Ensemble Model , 1992 .

[35]  Wojciech W. Grabowski,et al.  Cloud-resolving modeling of cloud systems during Phase III of GATE. Part II: Effects of resolution and the third spatial dimension , 1998 .

[36]  Xiaoqing Wu,et al.  Long-Term Behavior of Cloud Systems in TOGA COARE and Their Interactions with Radiative and Surface Processes. Part I: Two-Dimensional Modeling Study , 1998 .