首页> 外文会议>Geospatial Information Science: Geoinformatics 2006; Proceedings of SPIE-The International Society for Optical Engineering; vol.6420 >A GIS-based spatial distribution modeling of seasonal precipitation using terrain variables in Zhejiang province, China
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A GIS-based spatial distribution modeling of seasonal precipitation using terrain variables in Zhejiang province, China

机译:基于GIS的浙江省基于GIS的季节降水空间分布模型。

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Precipitation is a function of many topographical features as well as geographical locations. The correlations between precipitation and topographical and geographical features can be used to improve estimation of precipitation distribution. In this paper, we built seasonal precipitation model based on GIS techniques in Zhejiang province in southeastern China. Terrain variables derived from the 1 km resolution DEM are used as predictors of the seasonal precipitation, using a regression-based approach. Variables used for model development include: longitude, latitude, elevation, and distance from the nearest coast, direction to the nearest coast, slope, aspect, and the ratio of land to sea within given radii. Seasonal precipitation data, for the observation period 1971 to 2000, were assembled from 59 meteorological stations. Precipitation data from 52 meteorological stations were used to initialize the regression model. The data from the other 7 stations were retained for model validation. Seasonal precipitation surfaces were constructed using the regression equations, and refined by kriging the residuals from the regression model and subtracting the result from the predicted surface. Latitude, elevation and distance from the sea are found to be the most effective predictors of local seasonal precipitation. Validation determined that regression plus kriging predicts mean seasonal precipitation with a coefficient of determination (R~2), between the estimated and observed values, of 0.546 (winter) and 0.895 (spring). A simple regression model without kriging yields less accurate results in all seasons.
机译:降水是许多地形特征和地理位置的函数。降水与地形和地理特征之间的相关性可用于改善降水分布的估计。本文基于GIS技术,建立了中国东南部浙江省的季节性降水模型。使用基于回归的方法,将分辨率为1 km的DEM衍生的地形变量用作季节降水的预测指标。用于模型开发的变量包括:经度,纬度,海拔和距最近的海岸的距离,到最近的海岸的方向,坡度,纵横比以及给定半径内的陆地与海洋的比率。从59个气象站收集了1971年至2000年观测期的季节性降水数据。来自52个气象站的降水数据用于初始化回归模型。保留了其他7个站的数据以进行模型验证。使用回归方程构建季节性降水面,并通过从回归模型中剔除残差并从预测面中减去结果来进行修正。纬度,海拔和与海洋的距离被发现是当地季节性降水的最有效预测因子。验证确定,回归加克里金法可预测平均季节性降水,其确定系数(R〜2)在估计值和观测值之间,为0.546(冬季)至0.895(春季)。没有克里金法的简单回归模型在所有季节中得出的结果都不那么准确。

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