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线性加权回归模型的高原山地区域降水空间插值研究 被引量:15

A Weighted Linear Regression Model for Precipitation Spatial Interpolation in Altiplano and Mountain Area
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摘要 在山地和高原区域,地形对降水影响比较显著。常规空间插值方法通常不考虑地形要素,插值精度有限。考虑到降水量与高程存在较强的相关关系,采用局部线性加权回归模型预测山地和高原区域的降水分布。推导了回归计算公式,并在ArcGIS 9.0中编程实现算法。选取美国德克萨斯州西北部地区进行局部线性加权回归空间插值,并与普通Kriging、倒距离加权法比较。误差分析表明:在地形复杂的地区,线性加权回归模型比传统方法有优势。 Precipitation is evidently influenced by the terrain in the altiplano and mountain areas, in which the common methods, such as Inverse Distance Weighted (IDW) , Kriging Statistics and Polynomial Approximation, can't effectively estimate the actual spatial distribution of precipitation. Elevation is a significant factor in precipitation and, on a given mountain slope, precipitation typically increases with elevation. Accordingly, a local weighted linear regression model (WLR) is introduced attempting to accurately interpolate precipitation in the altiplano and mountain areas. The linear regression of precipitation versus elevation for spatial interpolation method is implemented in ArcGIS 9.0 software using VBA programming. The weight of each precipitation observation is calculated by the distance between the estimated point and the observation point. Case study of precipitation interpolation in northwestern Texas shows that: (1) WLR model is better than the common methods such as Kriging and IDW in terms of MAE and RMSE of cross validation in altiplano and mountain areas for specific precipitation periods. (2) Due to the seasonal characteristics of the precipitation distribution, the precision of WLR interpolation varies in different periods of precipitation ; compared with the common methods, the WLR model is better than IDW and Kriging methods for August precipitation data and has no evident difference for January data. (3) In the complex terrain area, the WLR model has evident advantages over the common approaches, and in the relatively flat area the model matches the IDW method. Considering that precipitation is influenced by more geographic factors such as mountain slope, aspect and wind direction, it is expected to develop a multiple linear regression model for precipitation interpolation in the future studies.
出处 《地球信息科学》 CSCD 2008年第1期14-19,共6页 Geo-information Science
基金 河南省高等学校创新人才基金(2004-2009年度)
关键词 降水量 空间插值 线性加权回归模型 precipitation spatial interpolation weighted linear regression model
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  • 1朝伦巴根,和泰,刘廷玺.含水层渗透系数K的空间变异性研究[J].地质学报,1994,68(4):358-367. 被引量:29
  • 2朱求安,张万昌.流域水文模型中面雨量的空间插值[J].水土保持研究,2005,12(2):11-14. 被引量:27
  • 3王劲峰,李全林,陈锦标,陈红焱.地震趋势区划结构自适应模型[J].中国地震,1996,12(A00):78-88. 被引量:6
  • 4张朝生,章申,何建邦.长江水系沉积物重金属含量空间分布特征研究——地统计学方法[J].地理学报,1997,52(2):184-192. 被引量:183
  • 5周允华 中国科学院北京农业生态系统试验站.中国地区光合有效辐射能量和光量子通量的时空分布.农田作物环境实验研究[M].北京:气象出版社,1990.15-39.
  • 6Thornton P E, Running S W, White M A. Generating surfaces of daily meteorological variables over large regions of complex terrain. J. Hydeol, 1997, 190:214-251.
  • 7Luo Z, Wahba G, Johnson D R. Spatial-temporal analysis of temperature using smoothing spline ANOVA. J. Climate,1998, 11(1): 18-28.
  • 8Snell S E, Gopal S, Kaufman R K. Spatial interpolation of surface air temperatures using artificial neural networks: Evaluating their use for downscaling GCMs. J. Climate,2000, 13(5): 886-895.
  • 9Phillips D L, Dolph J, Marks D. A comparison of geostatistical procedures for spatial analysis of precipitation in mountainous terrain. Agric. For. Meteorol, 1992, 58:119-141.
  • 10Robeson S M, Janis M J. Comparison of temporal and unresolved spatial variability in multiyear time-averages of air temperature. Climate Res, 1998, 10(1): 15-26.

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