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A GIS-based spatial distribution modeling of seasonal precipitation using terrain variables in Zhejiang province, China

机译:浙江省地区季节降水的基于GIS的空间分布建模

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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。降水和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。本文采用了基于中国东南部GIS技术的季节降水模型。使用基于回归的方法,从1公里分辨率DEM派生的地形变量用作季节降水的预测因素。用于模型开发的变量包括:距离最近的海岸的经度,纬度,高度和距离,到最近的海岸,坡度,方面以及在给定的半径内的土地与海上的比率。 1971年至2000年观察期间的季节降水数据由59个气象站组装。 52个气象站的降水数据用于初始化回归模型。保留来自其他7站的数据以进行模型验证。使用回归方程构建季节性沉淀表面,并通过克格从回归模型克劳的残留物改进并从预测表面减去结果。纬度,海拔和距离海的距离是最有效的当地季节降水的预测因子。验证确定回归加克里格预测估计和观察值之间的测定系数(R〜2),0.546(冬季)和0.895(弹簧)之间的测定系数(R〜2)。没有Kriging的简单回归模型在所有季节中产生较低的准确结果。

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