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AGRICULTURAL DROUGHT ASSESSMENT IN LATIN AMERICA BASED ON A STANDARDIZED SOIL MOISTURE INDEX

机译:基于标准化土壤湿度指数的拉丁美洲农业干旱评估

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We propose a relatively simple, spatially invariant and probabilistic year-round Standardized Soil Moisture Index (SSMI) that is designed to estimate drought conditions from satellite imagery data. The SSMI is based on soil moisture content alone and is defined as the number of standard deviations that the observed moisture at a given location and timescale deviates from the longterm normal conditions. Specifically, the SSMI is computed by fitting a non-parametric probability distribution function to historical soil moisture records and then transforming it into a normal distribution with a mean of zero and standard deviation of one. Negative standard normal values indicate dry conditions and positive values indicate wet conditions. To evaluate the applicability of the SSMI, we fitted empirical and normal cumulative distribution functions (ECDF and nCDF) to 32-years of averaged soil moisture amounts derived from the Essential Climate Variable (ECV) Soil Moisture (SM) dataset, and compared the root-mean-squared errors of residuals. SM climatology was calculated on a 0:25 grid over Latin America at timescales of 1, 3, 6, and 12 months for the long-term period of 1979-2010. Results show that the ECDF fits better the soil moisture data than the nCDF at all timescales and that the negative SSMI values computed with the non-parametric estimator accurately identified the temporal and geographic distribution of major drought events that occurred in the study area.
机译:我们提出了一种相对简单,空间不变和概率的全年标准化土壤湿度指数(SSMI),旨在估算卫星图像数据的干旱条件。 SSMI仅基于土壤水分含量,被定义为所观察到的位置和时间尺度的标准偏差的数量,并且少量偏离较长的正常情况。具体地,通过将​​非参数概率分布函数拟合到历史土壤湿度记录,然后将其转化为正常分布,以零和标准偏差将其转化为正常分布来计算SSMI。负标准正常值表示干燥条件和正值表示潮湿条件。为了评估SSMI的适用性,我们将经验和正常的累积分布功能(ECDF和NCDF)拟合到32多年的平均土壤湿度量来自基本气候变量(ECV)土壤水分(SM)数据集,并将根系进行比较 - 平方的残差误差。在长期期间,在1979 - 2010年的长期期间,在0:25格拉丁队以0:25格,在拉丁美洲的0:​​25格网站上计算了SM气候学。结果表明,ECDF在所有时间尺度都比NCDF融合了土壤湿度数据,并且使用非参数估计器计算的负SSMI值准确地确定了研究区域发生的主要干旱事件的时间和地理分布。

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