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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Combining thin-plate spline interpolation with a lapse rate model to produce daily air temperature estimates in a data-sparse alpine catchment
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Combining thin-plate spline interpolation with a lapse rate model to produce daily air temperature estimates in a data-sparse alpine catchment

机译:将薄板样条插值与流逝速率模型组合,以产生数据稀疏的高山集水区的日常气温估计

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摘要

Insufficient availability of weather stations recording air temperature is a common problem in many alpine regions. The low station density combined with the high variability of air temperature means that interpolated fields based on simple or more complex interpolation techniques are unlikely to be representative of the real patterns of air temperature. In this study, a novel method was developed to tackle this problem, following initial investigation of lapse rate variability in the study domain: the alpine Clutha catchment, New Zealand. Owing to a series of complexities in lapse rate variability, a multi-layer approach was adopted to produce 1 km(2) daily fields of maximum (Tmax) and minimum air temperature (Tmin). The first layer of the Tmax and Tmin models was calculated using a trivariate thin-plate spline, which was constrained to the elevations of the continuous network to avoid unrealistic extrapolation. To compensate for missing continuous high elevation records, two lapse rate models were implemented to scale air temperature above the first layer. The two lapse rate models were based on the dominant processes driving lapse rate variation, which were found to be cold air ponding (Tmin) and spatial differences in relative humidity (Tmax). Independent station records were used to assess accuracy and compare the resultant fields to an existing product (the Virtual Climate Station Network) and a more conventional method based on a bivariate spline and a constant lapse rate. The validation revealed that the new methods developed here have led to a substantial improvement in producing spatial estimates of Tmax, with a mean root mean square error (RMSE) of 2.38 degrees C, while progress in regard to Tmin was more limited (mean RMSE of 2.93 degrees C). As such, this work demonstrates that inclusion of the driving processes controlling lapse rates in interpolation routines can lead to improvements in accuracy.
机译:记录空气温度的气象站不足是许多高山地区的常见问题。低站密度与空气温度的高变异性结合意味着基于简单或更复杂的内插技术的内插场不太可能代表空气温度的真实模式。在本研究中,开发了一种新的方法,以解决这一问题的解决问题,如研究领域的渗透率变异性:新西兰高山Clutha集水区。由于渗透率变异性的一系列复杂性,采用多层方法来生产最大(Tmax)和最小空气温度(Tmin)的1公里(2)个日间。使用触发薄板样条计算的Tmax和Tmin模型的第一层,其被限制为连续网络的升高以避免不切实际的外推。为了弥补缺失的连续高仰角记录,实施了两种流逝速率模型以缩放第一层上方的空气温度。这两个流逝速率模型基于驾驶流失率变化的主要过程,这被发现是冷空气池(Tmin)和相对湿度(Tmax)的空间差异。独立的站记录用于评估准确性并将所得字段与现有产品(虚拟气候站网络)和基于双变型样条和恒定流失率的更传统方法进行比较。验证透露,这里开发的新方法导致了产生Tmax的空间估计的大幅改善,其平均根均方误差(Rmse)为2.38摄氏度,而Tmin的进展更受限制(平均值2.93℃)。因此,这项工作表明,包含控制插值例程中的失效率的驾驶过程可能导致精度提高。

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