A Characterization of Tropical Transient Activity in the CAM3 Atmospheric Hydrologic Cycle

Abstract The Community Atmosphere Model version 3 (CAM3) is the latest generation of a long lineage of general circulation models produced by a collaboration between the National Center for Atmospheric Research (NCAR) and the scientific research community. Many aspects of the hydrological cycle have been changed relative to earlier versions of the model. It is the goal of this paper to document some aspects of the tropical variability of clouds and the hydrologic cycle in CAM3 on time scales shorter than 30 days and to discuss the differences compared to the observed atmosphere and earlier model versions, with a focus on cloud-top brightness temperature, precipitation, and cloud liquid water path. The transient behavior of the model in response to changes in resolution to various numerical methods used to solve the equations for atmospheric dynamics and transport and to the underlying lower boundary condition of sea surface temperature and surface fluxes has been explored. The ratio of stratiform to conve...

[1]  T. N. Krishnamurti,et al.  The status of the tropical rainfall measuring mission (TRMM) after two years in orbit , 2000 .

[2]  M. Takahashi Simulation of the Quasi‐Biennial Oscillation in a general circulation model , 1999 .

[3]  Robert A. Houze,et al.  Stratiform Rain in the Tropics as Seen by the TRMM Precipitation Radar , 2003 .

[4]  H. Hendon,et al.  The diurnal cycle of tropical convection , 1993 .

[5]  Ken Tanaka,et al.  Analysis of Global Cloud Imagery from Multiple Satellites , 1991 .

[6]  Louis J. Bajuk,et al.  Seasonal and Interannual Variations in Stratiform and Convective Clouds over the Tropical Pacific and Indian Oceans from Ship Observations , 1998 .

[7]  W. Collins,et al.  The Formulation and Atmospheric Simulation of the Community Atmosphere Model Version 3 (CAM3) , 2006 .

[8]  K. Trenberth,et al.  The Diurnal Cycle and Its Depiction in the Community Climate System Model , 2004 .

[9]  P. Arkin,et al.  On the Relationship between Satellite-Observed Cloud Cover and Precipitation , 1981 .

[10]  G. North,et al.  Comparison of TRMM rainfall retrievals with rain gauge data from the TAO/TRITON buoy array , 2003 .

[11]  W. Collins,et al.  The Formulation and Atmospheric Simulation of the Community Atmosphere Model: CAM3 , 2005 .

[12]  J. Janowiak,et al.  An Examination of the Diurnal Cycle in Oceanic Tropical Rainfall Using Satellite and In Situ Data , 1994 .

[13]  P. Rasch,et al.  Representation of Clouds and Precipitation Processes in the Community Atmosphere Model Version 3 (CAM3) , 2006 .

[14]  A. Dai Global Precipitation and Thunderstorm Frequencies. Part II: Diurnal Variations , 2001 .

[15]  James J. Hack,et al.  CCSM–CAM3 Climate Simulation Sensitivity to Changes in Horizontal Resolution , 2006 .

[16]  A. Scott Denning,et al.  Simulations of terrestrial carbon metabolism and atmospheric CO2 in a general circulation model: Part 1: Surface carbon fluxes , 1996 .

[17]  Robert G. Ellingson,et al.  Satellite determinations of the relationship between total longwave radiation flux and infrared window radiance , 1984 .

[18]  Thomas M. Smith,et al.  An Improved In Situ and Satellite SST Analysis for Climate , 2002 .

[19]  Xiaoliang Song,et al.  Underestimated tropical stratiform precipitation in the National Center for Atmospheric Research (NCAR) Community Climate Model (CCM3) , 2004 .

[20]  B. N. Meisner,et al.  The Relationship between Large-Scale Convective Rainfall and Cold Cloud over the Western Hemisphere during 1982-84 , 1987 .

[21]  Phillip A. Arkin,et al.  Spatial and Annual Variations in the Diurnal Cycle of Large-Scale Tropical Convective Cloudiness and Precipitation , 1987 .

[22]  Robert A. Houze,et al.  Cloud clusters and superclusters over the oceanic warm pool , 1993 .

[23]  Harry H. Hendon,et al.  Some Implications of the Mesoscale Circulations in Tropical Cloud Clusters for Large-Scale Dynamics and Climate , 1984 .

[24]  J. Janowiak,et al.  The Global Precipitation Climatology Project (GPCP) combined precipitation dataset , 1997 .

[25]  Elizabeth C. Kent,et al.  Global analyses of sea surface temperature, sea ice, and night marine air temperature since the late nineteenth century , 2003 .

[26]  Philip J. Rasch,et al.  Characteristics of Atmospheric Transport Using Three Numerical Formulations for Atmospheric Dynamics in a Single GCM Framework , 2006 .

[27]  Murry L. Salby,et al.  Diurnal Variations of Cloud Cover and Their Relationship to Climatological Conditions , 1996 .

[28]  W. Collins,et al.  Description of the NCAR Community Atmosphere Model (CAM 3.0) , 2004 .

[29]  R. Houze Stratiform precipitation in regions of convection : A meteorological paradox ? , 1997 .

[30]  J. Slingo,et al.  The Diurnal Cycle in the Tropics , 2001 .

[31]  Murry L. Salby,et al.  Equatorial wave activity derived from fluctuations in observed convection , 1994 .

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

[33]  F. Wentz A well‐calibrated ocean algorithm for special sensor microwave / imager , 1997 .

[34]  Misako Kachi,et al.  Comparison of Rainfall Products Derived from TRMM Microwave Imager and Precipitation Radar , 2002 .

[35]  David P. Jorgensen,et al.  Vertical Velocity Characteristics of Oceanic Convection , 1989 .

[36]  Patrick Minnis,et al.  Examination of the relationship between outgoing infrared window and total longwave fluxes using satellite data , 1991 .

[37]  Thomas L. Bell,et al.  Sampling of the Diurnal Cycle of Precipitation Using TRMM , 2002 .

[38]  J. Gamache,et al.  Diagnosis of Cloud Mass and Heat Fluxes from Radar and Synoptic Data , 1980 .

[39]  Robert F. Adler,et al.  A Satellite Infrared Technique to Estimate Tropical Convective and Stratiform Rainfall , 1988 .

[40]  Rolando R. Garcia,et al.  The excitation of equatorial waves by deep convection in the NCAR Community Climate Model (CCM3) , 2000 .

[41]  James J. Hack,et al.  Simulation of the Global Hydrological Cycle in the CCSM Community Atmosphere Model Version 3 (CAM3): Mean Features , 2006 .

[42]  P. Webster,et al.  A Coupled Ocean-Atmosphere System of SST Modulation for the Indian Ocean* , 2000 .

[43]  N. McFarlane,et al.  The Variability of Modeled Tropical Precipitation , 2004 .

[44]  K. Bowman,et al.  Diurnal cycle of tropical precipitation in a general circulation model , 2004 .

[45]  Liming Xu,et al.  A Trmm-Calibrated Infrared Rainfall Algorithm Applied Over Brazil , 2001 .

[46]  Robert Wood,et al.  Diurnal cycle of liquid water path over the subtropical and tropical oceans , 2002 .

[47]  James J. Hack,et al.  The Climate Sensitivity of the Community Climate System Model Version 3 (CCSM3) , 2006 .

[48]  P. Sardeshmukh,et al.  Local Time- and Space Scales of Organized Tropical Deep Convection , 2002 .