首页> 外文期刊>Journal of Applied Meteorology >Interpolation Errors in Wind Fields as a Function of Spatial and Temporal Resolution and Their Impact on Different Types of Kinematic Trajectories
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Interpolation Errors in Wind Fields as a Function of Spatial and Temporal Resolution and Their Impact on Different Types of Kinematic Trajectories

机译:风场的插值误差与时空分辨率的关系及其对不同类型运动轨迹的影响

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This paper discusses some of the uncertainties that influence kinematic trajectory calculations. The interpolation errors due to different interpolation schemes are examined by degrading high-resolution wind fields from a numerical weather predictionmodel with respect to space and time. Under typical circumstances, the greatest errors are due to temporal interpolation, followed by horizontal and vertical interpolation. Relative errors in the vertical wind are higher than those in the horizontal windcomponents. These errors are quite substantial and severely affect the accuracy of trajectories. For instance, a decrease of the temporal resolution from 3 to 6 h leads to average relative interpolation errors of 16% in the horizontal wind components and 40% in the vertical wind component. These errors cause mean transport deviations of 280 km for two-dimensional model-level trajectories and 600 k-m for three-dimensional trajectories after 96-h travel time. The substantial deviations for three-dimensional trajectories are due to the large interpolation errors of the vertical velocity component Although the three-dimensional trajectories are more sensitive to interpolation errors, for sufficiently (though not ideally) resolved wind fields they seem tobe superior to model-level trajectories. An intercomparison of three-dimensional, model-level, isentropic. and boundary layer trajectories is presented.
机译:本文讨论了影响运动轨迹计算的一些不确定性。通过从数值天气预报模型相对于空间和时间降低高分辨率风场,可以检查由于不同插值方案导致的插值误差。在典型情况下,最大的误差是由于时间插值,然后是水平和垂直插值。垂直风的相对误差高于水平风分量的相对误差。这些误差非常大,严重影响了轨迹的准确性。例如,时间分辨率从3小时降低到6小时会导致水平风分量的平均相对插值误差为16%,垂直风分量的平均相对插值误差为40%。这些错误导致二维模型级轨迹的平均运输偏差为280 km,而经过96小时后,三维轨迹的平均运输偏差为600 k-m。三维轨迹的实质偏差是由于垂直速度分量的较大插值误差引起的,尽管三维轨迹对插值误差更敏感,但对于足够(尽管不是理想的)解析风场,它们似乎优于模型-水平轨迹。三维模型级等熵的比对。并给出了边界层的轨迹。

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