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Stochastic interpolation of rainfall data from raingages and radar using linear co-kriging.

机译:使用线性协同克里格法对降雨和雷达降雨数据进行随机插值。

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摘要

Linear co-kriging was used to merge raingage measurements and radar rainfall data. To evaluate various co-kriging estimators, three experiments were performed. The first two are simulation experiments. Assuming high-quality radar rainfall fields and the rainfall fields generated from a stochastic space-time rainfall model as the ground-truth rainfall fields, raingage measurements and radar rainfall fields were generated with varying raingage network density and the error characteristics of radar rainfall. Ordinary and universal co-kriging estimators were then used to merge the raingage measurements and the radar rainfall data. Since raingages are usually sparse, the second-order statistics required for co-kriging can only be known with large uncertainty. The effect of the uncertainty and the sampling error of raingage measurements were also evaluated by co-kriging ground-truth rainfall data and radar rainfall data. The third is a real-world experiment. A physically based rainfall model was used to estimate the mean field, or the trend, of ground-level rainfall field. Modified simple co-kriging was then performed to merge the residual raingage measurements and the residual radar rainfall data. Ordinary and universal co-kriging estimators were also included for comparison purposes. The results show that linear co-kriging is potentially useful for merging raingage measurements and radar rainfall data. Under a range of raingage network densities and error characteristics of radar rainfall data, the gage-radar estimation using co-kriging is shown to consistently provide rainfall estimates that are better, in the minimum-error-variance sense, to the gage-only or the radar-only estimates alone over the life cycle of an oceanic convective storm. The magnitude of improvement is only minor. However, the consistency of the improvement by the gage-radar estimation, under the various conditions of the error characteristics of radar rainfall makes co-kriging an attractive tool in rainfall estimation.
机译:线性协同克里格用于合并测距和雷达降雨数据。为了评估各种协同克里格估算器,进行了三个实验。前两个是模拟实验。假设高质量的雷达降雨场和随机时空降雨模型产生的降雨场作为地面真实降雨场,则产生了具有不同的降雨网络密度和雷达降雨误差特性的雷达测量场和雷达场。然后使用普通和通用的共同克里格估计器来合并测距和雷达降雨数据。由于掠夺通常是稀疏的,因此只能在很大的不确定性的情况下才能知道共同克里金法所需的二阶统计量。还通过联合克里特地面降雨数据和雷达降雨数据来评估不确定性的影响和测量的采样误差。第三个是实际实验。使用基于物理的降雨模型来估算地面降雨场的平均场或趋势。然后执行修改后的简单共同克里金法,以合并剩余的掠夺测量和剩余的雷达降雨数据。出于比较目的,还包括了普通和通用协同克里格估计器。结果表明,线性协同克里格对于合并测距测量和雷达降雨数据可能很有用。在一定范围的雨量网络密度和雷达降雨数据的误差特征下,使用协克里金法进行的量具-雷达估计显示出一致的降雨估计,在最小误差方差意义上,仅使用量具或仅在海洋对流风暴的生命周期内仅使用雷达进行估算。改善的幅度很小。但是,在雷达降雨误差特性的各种条件下,通过量具-雷达估算进行的改进的一致性使得共同克里格法成为降雨估算中的一种有吸引力的工具。

著录项

  • 作者

    Seo, Dong-Jun.;

  • 作者单位

    Utah State University.;

  • 授予单位 Utah State University.;
  • 学科 Hydrology.
  • 学位 Ph.D.
  • 年度 1988
  • 页码 217 p.
  • 总页数 217
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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