Microphysical data and radar reflectivities (Ze, -15< Ze<10 dB) measured from flights during the NASA Tropical Clouds, Convection, Chemistry and Climate field program,are used to relate Ze at X- and W-band to measured ice water content, IWC. Because nearly-collocated Ze and IWC were each directly measured, Ze-IWC relationships could be developed directly. Using the PSDs and ice particle masses evaluated based on the direct IWC measurements, reflectivity-snowfall rate, Ze-S, relationships were also derived. For -15< Ze<10 dB, our relationships yield larger IWC and S than given by the retrievals and earlier relationships.
The sensitivity of radar reflectivity to particle size distribution and size-dependent mass, shape, and orientation introduces significant uncertainties in retrieved quantities since these factors vary substantially globally. To partially circumvent these uncertainties, a W-band Ze-S relationships is developed by relating four years of global CloudSat reflectivity observations measured immediately above the melting layer to retrieved rain rates at the base of the melting layer, The supporting assumptions are that the water mass flux is constant through the melting layer, that the air temperature is nearly 0°C, and that the retrieved rain rates are well-constrained. Where Ze>10 dB, this Ze-S, relationship conforms well to earlier relationships, but for Ze<10 dB, it yields higher IWC and S. Because not all retrieval algorithms estimate either or both IWC and S, we use a large aircraft-derived data set to relate IWC and S. The IWC can then be estimated from S, and visa versa.