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Comparison of Spatial Interpolation Methods on Meteorological Element of the Beijing-Tianjin-Hebei region

机译:京津冀地区气象要素空间插值方法的比较

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Spatial interpolation methods in common use primary include inverse distance weighted (IDW), spline function (Spline), Kriging and overall polynomial interpolation. Based on the data of the meteorological monitor data at 90 stations in the Beijing-Tianjin-Hebei region from 1961 to 2007, which involve precipitation, mean temperature, duration of sunshine of each month, the calculation according to different interpolation methods were generated. In order to investigate the optimization methods, the results were used to compare with the meteorological monitor data at the other 10 stations that did not participate in former interpolations. After the error analysis, spline method Tension is the most accurate model in the results of the monthly precipitation interpolation, IDW secondly. For example, the relative error of the stations that did not participate in the analysis is 8.61 in Tension while 9.03 in IDW on precipitation interpolation in January. So the Tension is the best method to calculate the precipitation in the region based on the monitor data. Overall polynomial interpolation has the highest accuracy in the results of the monthly average temperature and monthly duration of sunshine interpolation. For example, in overall polynomial interpolation the relative error of the monthly average temperature and monthly duration of sunshine interpolation is 10.82 and 2.02 in January. Obviously, overall polynomial interpolation can be used to obtain the raster data around the station. It can be improved to consider the region as a combined part which can be divided in to mountainous region and plain. In this way, local polynomial interpolation can be used to compare with other interpolation method. By choosing the most precise method that reflects the actual distribution, estimated value of each pixel was obtained in the study area which render agroclimate data basis of various kinds model on growth of plants and other applications and is useful to the development of precision agriculture.
机译:常用的主要空间插值方法包括反距离加权(IDW),样条函数(Spline),克里格(Kriging)和整体多项式插值。根据1961 — 2007年京津冀地区90个站点的气象监测数据,分别涉及降水,平均温度,每月的日照时间,根据不同的插值方法进行了计算。为了研究优化方法,将结果与未参与先前插值的其他10个站点的气象监测数据进行比较。经过误差分析后,样条法张紧度是每月降水插值结果中最准确的模型,其次是IDW。例如,在一月份的降水插值中,未参与分析的站点的相对误差在Tension中为8.61,在IDW中为9.03。因此,张力是根据监测数据计算区域降水量的最佳方法。总体多项式插值在月平均温度和每月日照插值的结果中具有最高的准确性。例如,在整体多项式插值中,一月份月平均温度和日照插值的每月持续时间的相对误差为10.82和2.02。显然,整体多项式插值可用于获取测站周围的栅格数据。将区域视为可以分为山区和平原的组合部分可以进行改进。这样,可以使用局部多项式插值与其他插值方法进行比较。通过选择反映实际分布的最精确方法,在研究区域获得了每个像素的估计值,为植物生长和其他应用提供了各种模型的农业气候数据基础,对发展精确农业很有帮助。

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