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首页> 外文期刊>Journal of Applied Meteorology and Climatology >Retrieval of Snow Properties for Ku- and Ka-Band Dual-Frequency Radar
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Retrieval of Snow Properties for Ku- and Ka-Band Dual-Frequency Radar

机译:Ku和Ka波段双频雷达的降雪特性检索

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The focus of this study is on the estimation of snow microphysical properties and the associated bulk parameters such as snow water content and water equivalent snowfall rate for Ku- and Ka-band dual-frequency radar. This is done by exploring a suitable scattering model and the proper particle size distribution (PSD) assumption that accurately represent, in the electromagnetic domain, the micro-/macrophysical properties of snow. The scattering databases computed from simulated aggregates for small-to-moderate particle sizes are combined with a simple scattering model for large particle sizes to characterize snow-scattering properties over the full range of particle sizes. With use of the single-scattering results, the snow retrieval lookup tables can be formed in a way that directly links the Ku- and Ka-band radar reflectivities to snow water content and equivalent snowfall rate without use of the derived PSD parameters. A sensitivity study of the retrieval results to the PSD and scattering models is performed to better understand the dual-wavelength retrieval uncertainties. To aid in the development of the Ku- and Ka-band dual-wavelength radar technique and to further evaluate its performance, self-consistency tests are conducted using measurements of the snow PSD and fall velocity acquired from the Snow Video Imager/Particle Image Probe (SVI/PIP) during the winter of 2014 at the NASA Wallops Flight Facility site in Wallops Island, Virginia.
机译:这项研究的重点是估算雪的微观物理特性以及相关的体积参数,例如Ku和Ka频段双频雷达的雪水含量和水当量降雪率。这是通过探索合适的散射模型和适当的粒度分布(PSD)假设来完成的,这些假设在电磁域中可以准确表示雪的微观/宏观物理特性。从模拟聚集体计算出的中小粒径的散射数据库与大粒径的简单散射模型相结合,以表征整个粒径范围内的雪散射特性。利用单散射结果,可以形成雪检索表,而无需使用派生的PSD参数,就可以将Ku和Ka波段雷达的反射率直接与雪水含量和等效降雪率联系起来。对PSD和散射模型的检索结果进行了敏感性研究,以更好地理解双波长检索的不确定性。为了帮助发展Ku和Ka波段双波长雷达技术并进一步评估其性能,使用了从Snow Video Imager / Particle Image Probe获得的雪PSD和跌落速度的测量进行了自洽测试。 (SVI / PIP)在2014年冬季在美国弗吉尼亚州瓦洛普斯岛的NASA瓦洛普斯飞行设施站点上运行。

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