摘要
为研究福建省多年平均降水量的空间分布格局,为工农业生产、自然灾害预测、生态环境建设提供科学依据,利用福建省及周边区域35个气象站点1951—2011年降水资料,分析年均降水量与海拔、纬度、距海岸距离、坡向的相关性;同时,结合多元回归方程和克里金插值构建降水空间估算模型,反映出年均降水量空间分布的总体趋势,突出局部地区降水的差异,估算福建省1951—2011年年均降水量空间分布。结果表明:已知气象站点年均降水量估算的平均相对误差为3.4%,绝对误差为56 mm,验证站点的平均相对误差为3.6%;福建省年均降水量从东南沿海向西北山区呈现波动式上升的特点。
The aim of this research is to estimate the spatial distribution of annual mean precipitation in Fujian Province,hence offering scientific basis for industrial and agricultural production,natural disaster forecasting,and ecoenvironmental construction.According to precipitation data at 35 meteorological stations in Fujian province and its surrounding areas,the correlation between annual precipitation and four geological factors respectively (elevation,latitude,distance to sea shore,and slope gradient) were analyzed.Furthermore,a model was established in association with the multiple regression equation and the Kriging interpolation to estimate the spatial distribution of annual mean precipitation in Fujian Province from 1951 to 2011.The model reflects the general trend of the spatial distribution of annual precipitation,and also highlights the difference of precipitation in local areas.Results revealed that the relative average error of the fitted stations is 3.4%,and the mean absolute error is 56 mm; while the mean absolute error of the precision verification result is 3.6%.The annual precipitation displayed a wave-like rising trend from the southeast coast to the northwest mountains.
出处
《长江科学院院报》
CSCD
北大核心
2017年第10期11-16,共6页
Journal of Changjiang River Scientific Research Institute
关键词
地理因子
年降水量
回归拟合
克里金插值
空间分布
福建省
surface sediment
Bellamya
heavy metal
rsk assessment
environmental governance of Chaohu Lake