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顾及潮汐传播方向的多站水位线性内插方法
Linear Interpolation Method of Multi-Station Water Level Considering Tidal Propagation Direction
  
DOI:doi:10.3969/j.issn.1003-2029.2025.05.004
中文关键词:  水位改正  线性内插  时差法  差比法  潮汐传播方向
英文关键词:water level correction  linear interpolation  time difference method  range ratio method  propagation direction
基金项目:
作者单位
高兴国,曲萌,丁加豪,卜宪海 山东电力工程咨询院有限公司山东科技大学测绘与空间信息学院 
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中文摘要:
      针对常规线性内插水位模型未考虑潮汐的传播方向导致水位精度较低的问题,本文提出一种顾及潮汐传播方向的线性内插方法。首先,基于测区验潮站同步观测数据,利用三个验潮站之间的潮汐传播时差,推导了潮汐传播方向;然后,在顾及潮汐的传播方向后,对常规线性内插模型进行改进,进而计算更为精确的水位数据。实验结果表明:在本文实验数据下,当潮汐性质接近时,常规线性内插法获取的水位数据的误差约为±12.5 cm,在顾及潮汐的传播方向后,水位误差约为±3 cm,精度提升约70%,其精度水平与时差法、差比法接近;当潮汐性质相差较大,常规线性内插法获取的水位数据的误差约为±65 cm,经本文方法改正后,水位误差约为±5 cm,精度提升明显。所提方法可有效弥补传统线性内插法的局限性,对提高传统线性内插法的适用性具有一定参考意义。
英文摘要:
      To address the issue that the traditional linear interpolation water level model exhibits low accuracy due to its neglect of tidal propagation direction, this paper presents a linear interpolation method incorporating tidal propagation direction. Firstly, based on synchronous observation data from tide gauge stations in the survey area, the propagation direction of tidal waves is derived by analyzing the tidal propagation time differences among three stations. Subsequently, a propagation direction correction term is introduced into the classical linear interpolation model to construct a water level interpolation model accounting for tidal wave propagation characteristics, enabling high-precision water level calculation. Experimental results demonstrate that: when tidal properties in the survey area are similar, the water level error of the traditional linear interpolation method approximately ranges ±12.5 cm, which is reduced to ±3 cm after propagation direction correction, representing an approximately 70% improvement in accuracy comparable to the time-difference method and difference-ratio method; when significant tidal property variations exist across the region, the error of the traditional method expands to ±65 cm, whereas the proposed method controls the error within ±5 cm, showcasing remarkable accuracy enhancement. This approach effectively overcomes the limitations of traditional linear interpolation models and provides a novel technical pathway for improving the applicability of tidal level interpolation methods.
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