基于地统计学的气候变量空间插值应用——以甘肃省为例

Wenze Yue, Jianhua Xu, Hongjuan Liao, Lihua Xu
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引用次数: 4

摘要

摘要在回顾地质统计学的起源、发展和基本原理的基础上。本文主要介绍了两种插值方法:普通克里格法和共同克里格法。本文以甘肃省1961 - 1990年30年平均降水和蒸发量资料为例,探讨了基于地质统计学的气候变量空间插值方法。根据不同的半变异函数理论模型,分别采用普通克里格和二元克里格插值方法,并对研究结果进行比较。结果表明:(1)30年平均降水和蒸发量在空间上均呈现明显的梯度变化,且变化幅度较大。但前者的规模要大于后者。30年平均降水量由东南向西北逐渐减少,蒸发量由东南向西北逐渐增加。(2)根据半变异图云图和实验方差最小原理,选择合适的基于地统计学插值的理论半变异图模型,较好地模拟了特殊区划变量的空间连续分布格局。与普通克里格法相比,Cokriging法考虑了海拔高度对降水和蒸发的影响,因此具有更高的插值精度。(3)地统计学方法虽然能较好地反映气候变量的一般空间格局,但其插值精度并不高,有待进一步提高。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Applications of Spatial Interpolation for Climate Variables Based on Geostatistics: A Case Study in Gansu Province, China
Abstract Based on reviewing the origin, development and basic principles of Geostatistics. this article mainly introduces two interpolation methods: Ordinary Kriging and Cokriging. As an optimal one among so many methods to spatial interpolation for climate variables is not available, the article discusses Geostatistics-based interpolation methods by using 30-year average precipitation and evaporation data in Gansu province from 1961 to 1990. According to different semivariogram theory models, we adopt Ordinary Kriging and Bivariate Cokriging interpolation methods, and compare research results. We draw the following conclusions: (1) Both 30-year average precipitation and evaporation present obvious gradient change on space, in a great range. But the former's is larger than the latter's. 30-year average precipitation decreases gradually from southeast to northwest, however, evaporation increases gradually from southeast to northwest. (2) According to semivariogram cloud plots and experiment variance minimum principle, we select suitable theoretical semivariogram models based on Geostatistics interpolation, which can simulate the spatially continuous distribution patterns of the special regionalized variables in a better way. Compared with Ordinary Kriging, Cokriging considers the influence of altitude on precipitation and evaporation and thereby has higher interpolation accuracy. (3) Though Geostatistics methods can better reflect the general space patterns of climate variables, their interpolations precision is not high as we expect and can be improved further.
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