Radar observations of the kinematic, microphysical, and precipitation characteristics of two MCSs in TRMM LBA

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Environmental Characteristics of Convective Systems during TRMM-LBA (2002, background): “stratiform rainfall and weak convection nearly devoid of lightning (Cifelli et al., 2001;Williams et al., 1992).”
The 29 June 2000 Supercell Observed during STEPS. Part I: Kinematics and Microphysics (2005, methodology): “The original CHILL and S-Pol polarimetric data were first edited to eliminate noise, clutter, and suspect data using thresholds in hv and the standard deviation of dp. These methods have been described in Ryzhkov and Zrnic ´ (1998) and used in studies such as Carey and Rutledge (1996, 1998, 2000) an”
Mesoscale convective systems (2004, unknown): “The South American MCSs have been investigated with polarimetric radar in recent field studies [e.g., Cifelli et al., 2002].”
Detection of tropical deep convective clouds from AMSU-B water vapor channels measurements (2005, methodology): “[14] In order to confirm the criteria derived from the observations taken from TRMM LBA, one deep convective cloud system and one convective overshooting system observed during CAMEX-3 are analyzed.”
Evaluation of the diurnal cycle of precipitation, surface thermodynamics, and surface fluxes in the ECMWF model using LBA data (2002, unknown): “D20, 8045, doi:10.1029/2001JD000427, 2002 LBA 12 - 1 2000; Rickenbach et al., 2002; Cifelli et al., 2002].”