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Precipitation Regime Classification Based on Cloud-Top Temperature Time Series for Spatially-Varied Parameterization of Precipitation Models

机译:基于云层温度时间序列的降水制度分类,用于降水模型的空间变化参数化

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摘要

Satellite and reanalysis precipitation products perform poorly over regions with low-density ground observation networks. In order to improve space-dependent parameterization of precipitation estimation models in data-scarce environments, the delineation boundaries of precipitation regimes should be accurately identified. Existing approaches to characterize precipitation regimes by seasonal or other climatological properties do not account for small scale spatial-temporal variability. Precipitation time series can be used to account for this small-scale variability in regime classification. Unfortunately, precipitation products with global coverage perform poorly at small time scales over data scarce regions. A methodology of using satellite-based cloud-top temperature (CTT) time series as a proxy of precipitation time series for precipitation regime classification was developed, and its potential and uncertainty were analyzed. A precipitation regime in this study was defined on the basis of characteristic small-scale temporal distribution and variability of precipitation at a given place. Dynamic time warping was used to calculate the distance between two time series. Criteria to select the optimal temporal scale of time series for clustering and the number of clusters were also developed. The method was validated over Germany and applied to Tanzania, characterized by complex climatology and low density ground observations. This approach was evaluated against precipitation regime classification based on a satellite precipitation product. Results show that CTT outcompetes satellite-based precipitation for classification of precipitation regime classification. The CTT-based classification can be used as precursor to spatially adapted precipitation estimation algorithms where parameters are calibrated by gauge data or other ground-based precipitation observations, and parameterization can be used for satellite-precipitation estimates, precipitation forecasts in numerical or stochastic weather models, etc.
机译:卫星和再分析沉淀产品在具有低密度地面观察网络的区域上表现不佳。为了改善数据稀缺环境中降水估计模型的空间依赖性参数化,应准确识别降水制度的描绘边界。通过季节性或其他气候属性来表征降水制度的现有方法不考虑小规模的空间 - 时间可变性。降水时间序列可用于考虑该制度分类中的这种小规模变异性。不幸的是,具有全球覆盖率的降水产品在少时缩小数据稀缺地区时表现不佳。开发了使用卫星基云 - 顶温(CTT)时间序列作为降水调节分类的降水时间序列代理的方法,分析了其潜在和不确定性。本研究中的降水制度是基于特征小规模的时间分布和给定的地方降水的可变性来定义。动态时间翘曲用于计算两个时间序列之间的距离。还开发了选择聚类时间序列最佳时间序列的标准和集群的数量。该方法在德国验证并应用于坦桑尼亚,其特征在于复杂的气候学和低密度地面观察。根据卫星沉淀产品评估这种方法,避免沉淀制度分类。结果表明,CTT脱个于卫星基于卫星沉淀的降水制度分类。基于CTT的分类可以用作空间适应的降水估计算法,其中通过量规数据或其他地面沉淀观察校准参数,并且参数化可用于卫星降水估计,数值或随机天气模型中的降水预测, 等等。

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