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Analysis of bioclimatic time series and their neural network-based classification to characterise drought risk patterns in South Italy

机译:分析生物气候时间序列及其基于神经网络的分类,以表征意大利南部的干旱风险模式

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摘要

A new approach to characterise geographical areas with a drought risk index (DRI) is suggested, by applying an artificial neural network (ANN) classifier to bioclimatic time series for which operational temporal units (OtUs) are defined. A climatic database, corresponding to a grid of 8 km x 8 km cells covering the Italian peninsula, was considered. Each cell is described by the time series of seven variables recorded from 1989 to 2000. Sixteen cells were selected according to land cover homogeneity and completeness of the time series data. The periodic components of the time series were calculated by means of the fast Fourier transform (FFT) method. Temporal units corresponding to the period of the sinusoidal functions most related to the data were used as OtUs. The ANN for each OtU calculates a DRI value ranging between -1 and 1. The value is interpretable as the proximity of the OtUs to one of two situations corresponding to minimum and maximum drought risk, respectively. The former set (DRI = -1) is represented by an ideal OtU with minimum values of temperatures and evapo-transpiration, and maximum values of rainfall, normalised difference vegetation index (NDVI) and soil water content. The second set (DRI = 1) is represented by the reciprocal OtU to the former one. The classification of the cells based on DRI time profiles showed that, at the scale used in this work, DRI has no dependence on land cover class, but is related to the location of the cells. The methodology was integrated with GIS (geographic information system) software, and used to show the geographic pattern of DRI in a given area at different periods.
机译:通过将人工神经网络(ANN)分类器应用于定义了操作时间单位(OtU)的生物气候时间序列,提出了一种用干旱风险指数(DRI)表征地理区域的新方法。考虑了一个气候数据库,该数据库对应于覆盖意大利半岛的8 km x 8 km的网格。每个单元格由从1989年到2000年记录的七个变量的时间序列描述。根据土地覆盖的均匀性和时间序列数据的完整性选择了十六个单元格。时间序列的周期分量是通过快速傅立叶变换(FFT)方法计算的。与数据最相关的正弦函数周期的时间单位被用作OtU。每个OtU的ANN计算的DRI值介于-1和1之间。该值可解释为OtU分别对应于最小和最大干旱风险的两种情况之一的接近程度。前一组(DRI = -1)用理想的OtU表示,其理想值是温度和蒸散量的最小值,而降雨量的最大值,归一化植被指数(NDVI)和土壤含水量则是最大值。第二组(DRI = 1)由前一组的倒数OtU表示。根据DRI时间剖面对单元进行分类显示,在这项工作中使用的规模上,DRI不依赖于土地覆盖类别,而是与单元的位置有关。该方法与GIS(地理信息系统)软件集成在一起,用于显示指定区域内不同时期DRI的地理格局。

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