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Accounting for elevation and distance to the nearest coastline in geostatistical mapping of average annual precipitation

机译:在年平均降水量的地统计图中考虑海拔和到最近海岸线的距离

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Spatial distribution of precipitation in mountainous areas suggests strong control of surface orography on precipitation processes. Generally, quantifying orographic control of precipitation and identifying homogeneous areas are difficult because of the complex combination of factors, which could influence the precipitation process. The objective of this study was to account for morphometric attributes (elevations and distances to the nearest coastline) in geostatistical mapping of average annual precipitation in southern Italy. The study area was the Calabria Region, which has a spatially variable Mediterranean climate because of its high orographic variability. In this study, annual precipitation data collected by the former Italian Hydrographic Service for the 1916-2006 period were used. Elevations and distances to the nearest coastline were derived from a digital elevation model with 250 m x 250 m cell size in a geographic information system environment and used to delineate areas with homogeneous morphological features [landscape units (LU)]. The effectiveness of LU was assessed estimating the expected value of the average annual precipitation with polygon kriging and comparing their differences with the Mann-Whitney-Wilcoxon test. The average annual precipitation map showed that mountains areas receive more precipitation than low elevation areas and, in the Tyrrhenian side, it was also evident the orographic influence of Coastal chain on precipitation with high precipitation values. Results can help in understanding the differences among LU and the influence of surface orography on spatial patterns of annual precipitation in mountainous regions.
机译:山区降水的空间分布表明,对降水过程的表面地形有很强的控制作用。通常,由于因素的复杂组合,可能难以量化降水的地形控制和确定均匀区域,这可能会影响降水过程。这项研究的目的是在意大利南部年平均降水量的地统计学图中考虑形态特征(海拔和到最近海岸线的距离)。研究区域是卡拉布里亚地区,该地区由于地形变异性高而在空间上具有地中海气候。在这项研究中,使用了由前意大利水文局收集的1916-2006年期间的年降水量数据。到最近海岸线的海拔和距离是从地理信息系统环境中具有250 m x 250 m像元大小的数字海拔模型得出的,并用于描绘具有均一形态特征的区域[景观单位(LU)]。通过多边形克里格法评估了LU的有效性,以估计平均年降水量的期望值,并将其差异与Mann-Whitney-Wilcoxon检验进行比较。年平均降水量图显示,山区比低海拔地区的降水更多,在第勒尼安一侧,也很明显地看到沿海链对高降水量降水的地形影响。结果可以帮助了解LU之间的差异以及地表地形对山区年降水量空间格局的影响。

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