This paper describes the progress on a new project that is in the process of digitizing radar signals from eight channels on the phased array antenna at the National Weather Radar Testbed (NWRT) in Norman, Oklahoma. At the current time, a single-channel digital receiver is operational to mimic the current WSR-88D capability. The multi-channel digital data will foster a new generation of adaptive/fast scanning techniques and space-antenna nterferometry measurements, which will then be used to improve numerical weather prediction via data assimilation. Differing from the conventional rotating radar, the phased array is suited for multi-mission capabilities so that a variety of targets may be observed simultaneously with a high degree of fidelity. The development of this receiver will be an enabling tool for related research for the next decade.

Instrumentation of the Phased Array Radar system with a multi-channel receiver suite will bring out the full creativity of researchers using advanced techniques for maximizing the information from radar observations, as well as using them optimally in numerical models to improve weather prediction. The multi-channel receiver will collect signals from the sum, azimuth-difference, elevation-difference, and five broad-beamed auxiliary channels. One of the major advantages of the NWRT is the capability to adaptively scan weather phenomena at a higher temporal resolution than is possible with the WSR-88D. Hemispherical coverage in 1 min or less vs. 4 min, can be accomplished without comprising data accuracy. The multi-channel receiver will allow the direct implementation of interferometry techniques to measure crossbeam wind, shear and turbulence within a radar resolution volume. Access to the auxiliary channels will enable clutter mitigation and advanced array processing for high data quality with short dwell times. Potential benefits of high quality and high resolution data together with cross-beam wind, shear and turbulence include better understanding of storm dynamics and convective initiation, as well as better detection of small-scale phenomena including tornado and microburst, ultimately leading to increased lead time for warnings, and improved weather prediction.

The project is a collaborative effort between university and federal scientists. Assembly and testing of the instrument will be accomplished in the OU Atmospheric Radar Research Center (ARRC)'s Radar Innovation Laboratory (RIL) prior to integration into the NWRT. Scientists from the National Severe Storms Laboratory (NSSL) will take an active role in the integration of this instrument. The full conference paper will discuss this new project at OU in greater detail, which includes: advanced meteorological applications, predicted laboratory findings, initial designs and future risk mitigation strategies. A timeline for the subsequent work will also be discussed.