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The efficacy of Kriging spatial interpolation for filling temporal gaps in daily air temperature data:A case study in northeast China

机译:克里格空间插值方法在填补每日气温数据时空空白方面的功效:以东北地区为例

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摘要

Quality-controlled and serially complete daily air temperature data are essential to evaluating and modelling the influences of climate change on the permafrost in cold regions. Due to malfunctions and location changes of observing stations, temporal gaps (i.e., missing data) are common in collected datasets. The objective of this study was to assess the efficacy of Kriging spatial interpolation for estimating missing data to fill the temporal gaps in daily air temperature data in northeast China. A cross-validation experiment was conducted. Daily air temperature series from 1960 to 2012 at each station were estimated by using the universal Kriging (UK) and Kriging with an external drift (KED), as appropriate, as if all the ob-servations at a given station were completely missing. The temporal and spatial variation patterns of estimation uncer-tainties were also checked. Results showed that Kriging spatial interpolation was generally desirable for estimating missing data in daily air temperature, and in this study KED performed slightly better than UK. At most stations the cor-relation coefficients (R2) between the observed and estimated daily series were >0.98, and root mean square errors (RMSEs) of the estimated daily mean (Tmean), maximum (Tmax), and minimum (Tmin) of air temperature were <3 °C. However, the estimation quality was strongly affected by seasonality and had spatial variation. In general, estimation uncertainties were small in summer and large in winter. On average, the RMSE in winter was approximately 1 °C higher than that in summer. In addition, estimation uncertainties in mountainous areas with complex terrain were significantly larger than those in plain areas.
机译:质量评估和连续完整的每日气温数据对于评估和模拟气候变化对寒冷地区多年冻土的影响至关重要。由于观测站的故障和位置变化,在收集的数据集中普遍存在时间间隙(即丢失数据)。这项研究的目的是评估克里格空间插值法在估计缺失数据以填补中国东北地区每日气温数据的时间空白方面的功效。进行了交叉验证实验。通过使用通用Kriging(英国)和带有外部漂移的Kriging(KED)(视情况而定)来估计每个站从1960年到2012年的每日气温序列,就好像完全遗忘了给定站的所有观测结果一样。还检查了估计不确定度的时间和空间变化模式。结果表明,通常需要使用Kriging空间插值法来估计每日气温中的缺失数据,并且在这项研究中,KED的性能略好于UK。在大多数站点,观测和估计的每日序列之间的相关系数(R2)> 0.98,并且估计的每日平均值(Tmean),最大(Tmax)和最小(Tmin)的均方根误差(RMSE)空气温度<3°C。但是,估计质量受到季节的强烈影响并且具有空间差异。通常,估计不确定性在夏季较小,而在冬季较大。平均而言,冬季的RMSE比夏季高约1°C。此外,地形复杂的山区的估计不确定性明显大于平原地区。

著录项

  • 来源
    《寒旱区科学(英文版)》 |2016年第5期|441-449|共9页
  • 作者单位

    National-Local Joint Engineering Laboratory of Geo-Spatial Information Technology, Hunan University of Science and Technology, Xiangtan, Hunan 411201, China;

    National-Local Joint Engineering Laboratory of Geo-Spatial Information Technology, Hunan University of Science and Technology, Xiangtan, Hunan 411201, China;

    National-Local Joint Engineering Laboratory of Geo-Spatial Information Technology, Hunan University of Science and Technology, Xiangtan, Hunan 411201, China;

    State Key Laboratory of Frozen Soils Engineering, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China;

    State Key Laboratory of Frozen Soils Engineering, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China;

  • 收录信息 中国科学引文数据库(CSCD);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
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  • 入库时间 2022-08-19 03:41:29
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