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A Climatology of Disdrometer Measurements of Rainfall in Finland over Five Years with Implications for Global Radar Observations

机译:五年来芬兰的测雨量计气候学研究对全球雷达观测的意义

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摘要

To improve the understanding of high-latitude rain microphysics and its implications for the remote sensing of rainfall by ground-based and spaceborne radars, raindrop size measurements have been analyzed that were collected over five years with a Joss-Waldvogel disdrometer located in Jarvenpaa, Finland. The analysis shows that the regional climate is characterized by light rain and small drop size with narrow size distributions and that the mutual relations of drop size distribution parameters differ from those reported at lower latitudes. Radar parameters computed from the distributions demonstrate that the high latitudes are a challenging target for weather radar observations, particularly those employing polarimetric and dual-frequency techniques. Nevertheless, the findings imply that polarimetric ground radars can produce reliable "ground truth" estimates for space observations and identify dual-frequency radars utilizing a W-band channel as promising tools for observing rainfall in the high-latitude climate.
机译:为了增进对高纬度雨水微观物理学的理解及其对地面和星载雷达对雨量遥感的影响,对雨滴大小的测量结果进行了分析,这些测量值是使用位于芬兰耶尔文帕(Jarvenpaa)的Joss-Waldvogel测距仪在五年内收集的。分析表明,该区域气候的特征是小雨和小液滴,液滴分布窄,并且液滴大小分布参数的相互关系不同于低纬度地区。根据分布计算得出的雷达参数表明,高纬度是气象雷达观测的挑战性目标,尤其是那些采用极化和双频技术的观测。尽管如此,这些发现暗示着极化地面雷达可以为太空观测提供可靠的“地面真相”估计,并可以将利用W波段信道的双频雷达确定为在高纬度气候中观测降雨的有前途的工具。

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