NEXRAD or Nexrad (Next-Generation Radar) is a network of 158 high-resolution Doppler radars operated by the National Weather Service, an agency of the National Oceanic and Atmospheric Administration (NOAA) within the United States Department of Commerce. Its technical name is WSR-88D, which stands for Weather Surveillance Radar, 1988, Doppler. NEXRAD detects precipitation and atmospheric movement or wind. It returns data which when processed can be displayed in a mosaic map which shows patterns of precipitation and its movement. The radar system operates in two basic modes, selectable by the operator: a slow-scanning clear-air mode for analyzing air movements when there is little or no activity in the area, and a precipitation mode with a faster scan time for tracking active weather. NEXRAD has an increased emphasis on automation, including the use of algorithms and automated volume scans.
| VCP | Scan Time (min) | Elevation angles (°) | Usage | Special attributes |
|---|---|---|---|---|
| 11 | 5 | 0.5, 1.5, 2.4, 3.4, 4.3, 5.3, 6.2, 7.5, 8.7, 10, 12, 14, 16.7, 19.5 | Convection, especially when close to the radar | Has the best overall volume coverage. |
| 12 | 4 | 0.5, 0.9, 1.3, 1.8, 2.4, 3.1, 4.0, 5.1, 6.4, 8.0, 10.0, 12.5, 15.6, 19.5 | Convection, especially activity at longer ranges | Focuses on lower elevations to better sample the lower levels of storms. |
| 121 | 5.5 | 0.5, 1.5, 2.4, 3.4, 4.3, 6.0, 9.9, 14.6, 19.5 | Large number of rotating storms, tropical systems, or when better velocity data is needed. | Scans lower cuts multiple times with varying pulse repetitions to greatly enhance velocity data. |
| 21 | 6 | 0.50, 1.5, 2.4, 3.4, 4.3, 6.0, 9.9, 14.6, 19.5 | Shallow precipitation | Rarely used for convection due to sparse elevation data and long completion time. |
| 31 | 10 | 0.5, 1.5, 2.5, 3.5, 4.5 | Detecting subtle boundaries or wintry precipitation | Long-pulse |
| 32 | 10 | 0.5, 1.5, 2.5, 3.5, 4.5 | Slow rotation speed allows for increased sensitivity. Default clear-air mode, reduces wear on antenna. | Short-pulse |
The next major upgrade is likely to be polarimetric radar, which adds vertical polarization to the current horizontal radar waves, in order to more accurately discern what is reflecting the signal. This so-called dual polarization allows the radar to distinguish between rain, hail and snow, something the horizontally polarized radars cannot accurately do. Early trials have shown that rain, sleet, snow, hail, birds, insects, and ground clutter all have different signatures with dual-polarization, which could mark a significant improvement in forecasting winter storms and severe thunderstorms. *
Beyond dual-polarization, the advent of phased array radar will probably be the next giant leap in severe weather detection. Its ability to rapidly scan large areas would give an enormous advantage to radar meteorologists. Any large-scale installation by the NWS is unlikely to occur before the end of the decade. Such a system would more likely be installed separate from the existing WSR-88D network, perhaps only in areas like the Great Plains where tornadoes are more common.