Central Florida (MELB) was selected as one of four primary sites for TRMM GV operations, and is well complemented by several state-operated gauge networks, as well as a NASA-operated network at NASA Kennedy Space Center (KSC). More recently, with the participation of the University of Central Florida, two Joss-Waldvogel disdrometers have been sited near the radar, which are providing near-real-time estimates of the drop size distributions of precipitation. The principal radar is located on the eastern Atlantic seaboard in Melbourne, Florida. The area observed by the radar is approximately 50% ocean and 50% land. Florida is a sub-tropical location that receives about 70% of its annual rainfall between June and September. Most of this rainfall is due to sea breeze induced isolated convective systems, and more organized tropical systems. Florida's annual rainfall budget also receives a contribution from mid-latitude synoptic systems during northern hemispheric winter months when frontal boundaries occasionally affect the area. The diurnal cycle of rainfall at MELB is dominated by the frequent occurrence of sea breeze induced convection in the mid-to-late afternoon. This study will use the near decade-long record of observations to provide a climatology of precipitation over central Florida over daily, monthly, seasonal, and yearly scales, including the following: rain rate distributions, drop size distribution characteristics, reflectivity distributions. A discussion of the various statistics during passage of easterly wave, tropical storms, and hurricanes will also be provided.
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