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Improved long-term mean annual rainfall fields for Colombia

机译:哥伦比亚长期平均年降水量场的改善

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摘要

With the aim of improving the long-term mean annual surface water balance of Colombia, four new annual average precipitation fields are estimated at 4 km spatial resolution. To put in context, a concise literature review of rainfall in Colombia is presented. For estimation purposes, diverse multivariate geostatistical methods are implemented by combining information from 1180 raingauges covering the period 1950-2005, and satellite data from the tropical rainfall measuring mission (TRMM) for the period 1999-2005, used as a drift for the following geostatistical methods: (1) kriging with an external drift (KED), (2) standardized cokriging (SCK), (3) colocated cokriging (CCK), and (4) Markov regionalization CCK (CCKM). To ensure the reliability of the estimated precipitation fields, a detailed cross-validation procedure is performed, including univariate and bivariate analyses of residuals, which allows us to conclude that the best estimated rainfall field is obtained with KED, and the worst with SCK. Visual analyses are also performed in the search for consistency of the resulting precipitation fields. Furthermore, local (at-a-pixel) uncertainty modelling analysis is performed using the indicator approach. Conditional cumulative distribution functions (CCDF) are estimated using indicator CCK with Bayes-Markov hypothesis. Statistical descriptors for the pixel's CCDFs are estimated based on the resulting precipitation fields, including long-term mean, conditional variance and the coefficient of variation. These improved precipitation fields along with their estimated uncertainties are available for the scientific community and constitute useful basic information for diverse applications in water resources, agriculture, hydropower generation, human health, risks and disaster prevention, and many other applied sectors in Colombia.
机译:为了改善哥伦比亚的长期年平均地表水平衡,估计四个新的年平均降水场的空间分辨率为4 km。在上下文中,简要介绍了哥伦比亚的降雨情况。出于估计目的,通过将覆盖1950-2005年的1180个雨量计的信息与来自1999-2005年的热带雨量测量任务(TRMM)的卫星数据相结合,实现了多种多元地统计方法,这些数据被用作以下地统计的漂移方法:(1)外部漂移克里金法(KED),(2)标准化协同克里金法(SCK),(3)协同协同克里金法(CCK),以及(4)马尔可夫区域化CCK(CCKM)。为了确保估计的降水场的可靠性,执行了详细的交叉验证程序,包括对残差的单变量和双变量分析,这使我们可以得出结论:KED获得了最佳估计降雨场,而SCK获得了最差的降雨场。在寻找结果降水场的一致性方面,还进行了视觉分析。此外,使用指示符方法执行局部(一个像素)不确定性建模分析。条件累积分布函数(CCDF)使用带有贝叶斯-马尔可夫假设的指标CCK进行估算。像素的CCDF的统计描述符是根据产生的降水场估算的,包括长期平均值,条件方差和变异系数。这些改进的降水场及其估计的不确定性可供科学界使用,并为在水资源,农业,水力发电,人类健康,风险和防灾以及哥伦比亚许多其他应用领域的各种应用提供了有用的基本信息。

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