<p>The Marine Meteorology Division of the U.S. Naval Research Laboratory (NRL) has developed and transitioned a 3DVAR reflectivity data assimilation (DA) system into operations at Fleet Numerical Meteorology and Oceanography Center (FNMOC), located in Monterey, California.&#160; The system assimilates hourly, volumetric, radar reflectivity data into the Coupled Ocean/Atmosphere Mesoscale Prediction System (COAMPS<sup>&#174;</sup>)<sup>1</sup> high-resolution NWP model within the ship-following COAMPS &#8211; On demand System (COAMPS-OS<sup>&#174;</sup>)<sup>1</sup>.&#160; Both Next-Generation Radar (NEXRAD) land-based radar data and U.S. Navy shipboard SPS-48/Hazardous Weather Detection and Display Capability (HWDDC) radar data are assimilated depending on their data coverage provided to the COAMPS<sup>&#174;</sup> nested grids. The SPS-48/HWDDC units are installed on eighteen U.S. Navy aircraft carriers and amphibious assault ships, and when underway on a mission, the available units automatically transmit compressed, radar data files to FNMOC near the top of the hour.&#160; Through previously reported NRL and FNMOC demonstrations, and more recent operationally testing at FNMOC, the COAMPS-OS<sup>&#174; </sup>radar DA system&#8217;s nowcasting products have demonstrated their ability to provide improved predictions of precipitation events out to at least 6 hour forecasts compared to 3DVAR conventional DA into COAMPS<sup>&#174;</sup> alone.&#160; Shipboard SPS-48/HWDDC radar data and their assimilation into COAMPS-OS<sup>&#174;</sup> at FNMOC provide critical environmental awareness in the data sparse oceanic regions of the world that the Navy warfighter encounters.</p><p>The SPS-48 radar is a S-band, phased-array, azimuthally scanning, air-search radar that scans electronically in elevation and completes a volume scan in four seconds. The HWDDC combines the volume scans into motion-compensated, one-minute composites with limited clutter filtering applied. The SPS-48 beams are combined to yield full PPI scans at 22 different elevation angles ranging from 0.1&#176; to 24&#176;. The azimuthal resolution of the data is 1&#176; and the range resolution is 1 km. The maximum range for reflectivity (radial velocity) data is 250 (81) km. &#160;The Doppler data are only produced for the lowest three elevation scans whereas reflectivity data are produced for all elevation scans; all these data are archived in Universal Format and compressed before dissemination to FNMOC.&#160; &#160;Owing to the limited HWDDC Doppler data both in range and elevation, and the single-polarization of the SPS-48 radar waveform, reflectivity data quality control is particularly challenging.&#160; New algorithms have been developed to handle sea clutter and constant power function artifacts, such as bullseyes and sun strobes.&#160; There are two algorithms for sea clutter; the first one deals with anomolus propagation sea clutter caused by sea-water evaporation into the atmospheric surface layer, and the second one deals with the more widespread and distant sea clutter due to surface-based and elevated electromagnetic ducts resulting from trapped moist air under temperature inversions often encountered off the coasts of California and the Arabian Gulf region.&#160; An overview of the ship-following COAMPS-OS<sup>&#174; </sup>radar data quality control and assimilation system will be presented along with examples of quality controlled SPS-48/HWDDC radar data and the impact on COAMPS<sup>&#174;</sup> forecast skill scores.</p><p>&#160;</p><p><sup>1</sup> COAMPS and COAMPS-OS are registered trademarks of the U.S. Naval Research Laboratory</p>