Quantifying the Hydrometeorological Impacts of Lowering Operational Weather Radar Scan Elevation Angle

Liang-yu Wang, Haonan Chen
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Abstract

The operational Weather Surveillance Radar-1988 Doppler (WSR-88D) network forms the cornerstones of the national weather and climate observation infrastructure, to support forecast and warning operations, as well as aviation safety and flood mitigation systems. The current regulations limit the lowest elevation angle used by WSR-88D to 0.5°, i.e., one-half the antenna beamwidth. However, due to the Earth’s curvature and terrain blockage, more than 70% of the atmosphere below 1 km above ground level cannot be observed, especially when it is far from the radar stations. Unfortunately, that is where most severe weather hazards occur such as floods and tornadoes. Radar hydrometeorology observations and subsequent precipitation estimates will be closer to the ground if they are obtained at lower heights. Recently, the National Weather Service (NWS) has initiated a prototype demonstration of lowering the WSR-88D scan elevation angle to 0° or even lower. The KMUX WSR-88D radar in California is one of the first radar stations that have executed the lower elevation angle scan. Using the KMUX radar as an example, this study quantifies the hydrometeorological impacts of lowering WSR-88D scan elevation angle. In particular, the distribution of polarimetric radar measurements at 0° and 0.5° elevation angles are investigated to highlight the hydrometeor characteristics, especially when the 0.5° beam is shooting or overshooting the melting layer while the 0° beam is observing liquid precipitation regions close to the ground. The enhanced rainfall microphysical structures brought by the 0° scans are investigated to reveal the changes of precipitation during the falling processes. In addition, enhanced radar rainfall algorithms for local application in the San Francisco Bay Area are derived based on raindrop size distribution data, and the enhanced algorithms are compared with operational radar rainfall relations adopted by the WSR-88D systems.
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降低业务气象雷达扫描仰角对水文气象影响的量化
可操作的天气监视雷达-1988多普勒(WSR-88D)网络构成了国家天气和气候观测基础设施的基石,以支持预报和预警业务,以及航空安全和洪水缓解系统。目前的规定限制WSR-88D使用的最低仰角为0.5°,即天线波束宽度的一半。然而,由于地球的曲率和地形的阻塞,超过70%的地面以上1公里以下的大气无法被观测到,特别是当它远离雷达站时。不幸的是,那里是最严重的天气灾害发生的地方,如洪水和龙卷风。雷达水文气象观测和随后的降水估计如果在较低的高度获得,将更接近地面。最近,美国国家气象局(NWS)启动了将WSR-88D扫描仰角降低到0°甚至更低的原型演示。位于加州的KMUX WSR-88D雷达是首批执行低仰角扫描的雷达站之一。以KMUX雷达为例,量化了降低WSR-88D扫描仰角对水文气象的影响。特别是,研究了0°和0.5°仰角极化雷达测量值的分布,以突出水流星特征,特别是当0.5°波束射入或过射入熔化层时,而0°波束则观测接近地面的液体降水区域。研究了0°扫描带来的降雨微物理结构增强,揭示了降水过程中降水的变化。此外,基于雨滴大小分布数据推导了适合旧金山湾区局部应用的增强雷达降雨算法,并将增强算法与WSR-88D系统采用的实际雷达降雨关系进行了比较。
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