巴勒斯坦法利亚流域降雨制图插值方法的比较分析

A. Khader, A. Jayyousi, C. Chwala, H. Kunstmann, S. Shadeed
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引用次数: 1

摘要

降雨数据的可用性对于极端降雨事件的预测、水文建模和水资源系统的设计至关重要。在巴勒斯坦,现有的雨量计和雨量数据有限,不足以精确描述整个地区的面雨量分布。因此,必须找到适当的方法,利用现有雨量计的雨量资料,在某些没有雨量测量资料的地方预测雨量。本研究旨在确定最合适的插值方法,可用于在巴勒斯坦法里亚流域产生插值降雨面。法利亚集水区(320平方公里)位于巴勒斯坦西岸东北部,其特点是雨量时空变化大。第六,基于gis的空间插值方法通过视觉观察和交叉验证进行了测试。这些方法是:逆距离加权法、完全正则样条法、张力样条法、普通克里格法、通用克里格法和回归法。16个地点在两个雨季录得的雨量资料;使用了2016/2017和2017/2018。结果表明,通用克里格法在两个季节的相关系数略高,平均相对误差略小,是绘制法利亚流域降水分布的最优方法。此外,两季雨量的空间分布也影响了不同插值方法在流域内的效果。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Comparative analysis of interpolation methods for rainfall mapping in the Faria catchment, Palestine
The availability of rainfall data is essential for the prediction of extreme rainfall events, hydrological modeling, and the design of water resources systems. In Palestine, the limited available rain gauges and the available rainfall data are insufficient to precisely characterize the areal rainfall distribution over the entire area. Hence, it is essential to find proper methods to utilize the available rainfall data at the existing raingauges to predict rainfall values at certain locations where rainfall measurements are not available. This study aims at identifying the most suitable interpolation method that can be used to produce interpolated rainfall surfaces at the Faria catchment, Palestine. Faria catchment (320 km2), located in the northeastern part of the West Bank, Palestine, is characterized by high temporal and spatial rainfall variations. Six, GIS-based, spatial interpolation methods have been tested by visual observation and cross-validation. These methods are: Inverse Distance Weighted, Spline completely Regularized, Spline with Tension, Ordinary Kriging, Universal Kriging, and Regression. Available seasonal rainfall data recorded at 16 locations for two rainy seasons; 2016/2017 and 2017/2018 were utilized. Results indicate that the Universal Kriging method has slightly a higher correlation coefficient and lower mean relative error than the other methods for the two seasons that make the method the most optimal one for mapping rainfall distribution in the Faria catchment. Moreover, the spatial distribution of raingauges between the two seasons affects the performance of different interpolation methods in the catchment.
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