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首页> 外文期刊>Asia-Pacific journal of atmospheric sciences >Polarimetric Rainfall Retrieval from a C-Band Weather Radar in a Tropical Environment (The Philippines)
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Polarimetric Rainfall Retrieval from a C-Band Weather Radar in a Tropical Environment (The Philippines)

机译:在热带环境中通过C波段天气雷达进行极化雨量反演(菲律宾)

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摘要

We evaluated the potential of polarimetric rainfall retrieval methods for the Tagaytay C-Band weather radar in the Philippines. For this purpose, we combined a method for fuzzy echo classification, an approach to extract and reconstruct the differential propagation phase, Φ_(DP), and a polarimetric self-consistency approach to calibrate horizontal and differential reflectivity. The reconstructed Φ_(DP) was used to estimate path-integrated attenuation and to retrieve the specific differential phase, K_(DP). All related algorithms were transparently implemented in the Open Source radar processing software wradlib. Rainfall was then estimated from different variables: from re-calibrated reflectivity, from re-calibrated reflectivity that has been corrected for path-integrated attenuation, from the specific differential phase, and from a combination of reflectivity and specific differential phase. As an additional benchmark, rainfall was estimated by interpolating the rainfall observed by rain gauges. We evaluated the rainfall products for daily and hourly accumulations. For this purpose, we used observations of 16 rain gauges from a five-month period in the 2012 wet season. It turned out that the retrieval of rainfall from K_(DP) substantially improved the rainfall estimation at both daily and hourly time scales. The measurement of reflectivity apparently was impaired by severe miscalibration while K_(DP) was immune to such effects. Daily accumulations of rainfall retrieved from K_(DP) showed a very low estimation bias and small random errors. Random scatter was, though, strongly present in hourly accumulations.
机译:我们评估了菲律宾大雅台C波段天气雷达的极化降雨反演方法的潜力。为此,我们结合了一种用于模糊回波分类的方法,一种提取和重建差分传播相位Φ_(DP)的方法以及一种极化自洽方法来校准水平和差分反射率的方法。重建的Φ_(DP)用于估计路径积分衰减并检索特定的差分相位K_(DP)。所有相关算法均在开源雷达处理软件wradlib中透明实现。然后根据不同的变量估算降雨:根据重新校准的反射率,针对路径积分衰减进行了校正的重新校准的反射率,特定的微分相位,以及反射率和特定的微分相位的组合。作为另一个基准,通过对雨量计观测到的降雨量进行插值来估算降雨量。我们评估了每日和每小时累积的降雨产品。为此,我们使用了2012年雨季五个月内对16个雨量计的观测结果。事实证明,从K_(DP)检索降雨大大改善了每日和每小时时间尺度的降雨估计。反射率的测量显然由于严重的失准而受到损害,而K_(DP)不受这种影响。从K_(DP)取回的降雨的日累积量显示出非常低的估计偏差和较小的随机误差。但是,每小时的累积中强烈存在随机散布。

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  • 来源
    《Asia-Pacific journal of atmospheric sciences》 |2014年第novasuppla期|43-55|共13页
  • 作者单位

    University of the Philippines Diliman, National Institute of Geological Sciences, Quezon City, Philippines;

    Department of Civil Protection, Presidency of the Council of Ministers, Rome, Italy;

    University of the Philippines Diliman, National Institute of Geological Sciences, Quezon City, Philippines,University of Potsdam, Institute of Earth and Environmental Sciences, Potsdam, Germany;

    University of the Philippines Diliman, National Institute of Geological Sciences, Quezon City, Philippines;

    University of Potsdam, Institute of Earth and Environmental Sciences, Potsdam, Germany;

    University of Potsdam, Institute of Earth and Environmental Sciences, Potsdam, Germany,University of Potsdam, Institute of Earth and Environmental Sciences, Karl-Liebknecht-Str. 24-25,14476 Potsdam, Germany;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Dual-Pol; weather radar; quantitative precipitation estimation; differential propagation phase; attenuation; The Philippines;

    机译:双极;天气雷达定量降水估计;差分传播阶段;衰减;菲律宾人;

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