Estimate of precipitation from the dual-beam airborne radars in TOGA COARE. Part II: Precipitation efficiency in the 9 February 1993 MCS

Dual-beam airborne Doppler radars are commonly used in convection experimen ts for their ability to describe the dynamical structure of weather systems . However, instrumental limitations impose the use of wavelengths such as X -band, which are largely attenuated through heavy rain. This paper is the second of a series of two, which aim at developing scheme s for attenuation correction. The authors' final objective is to improve th e estimation of precipitation sampled from airborne radars. The first paper was dealing with the application of "differential algorithms'' ("stereorad ar'' and "quad beam'') to the independent retrieval of the specific attenua tion and nonattenuated reflectivity, which shed some light on the physics o f the precipitation. This second paper develops a more extensive procedure based upon the hybridization of a "differential'' and an "integral'' algori thm. It is much more flexible than the methods proposed in part one and all ows full rainfall-rate retrievals in single aircraft experiments. This proc edure is applied to the 9 February mesoscale convective system (MCS) study case from Tropical Ocean and Global Atmosphere Coupled Ocean-Atmosphere Res ponse Experiment (TOGA COARE), and the impact of the reflectivity correctio n on the water budget at the cloud system scale is discussed. As expected, the production of water in the 9 February squall line is maxim um below the freezing level and is located in the updraft resulting from th e interaction between the warm inflow and rear-to-front cold flow. The auth ors' analysis shows that the precipitation efficiency in the convective reg ion of the system is 31%. Therefore, the large majority of water vapor cond ensed into cloud droplets and ice crystals does not immediately reach the s urface as precipitation. It travels toward the rear of the system at the sp eed of the horizontal air motion, which suggests a large contribution of th e stratiform area in the global water budget. The same calculation performe d using raw attenuated data (without correcting scheme) gives an efficiency of only 19%. That result points out the importance of the correction for a ttenuation when measured reflectivities are used in rain-rate retrievals an d water budgets.