Estimation of Soil Moisture Percentage Using LANDSAT-based Moisture Stress Index

P. Welikhe, J. Quansah, S. Fall, W. McElhenney
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引用次数: 37

Abstract

The global agronomy community needs quick and frequent information on soil moisture variability and spatial trends in order to maximize crop production to meet growing food demands in a changing climate. However, in situ soil moisture measurement is expensive and labor intensive. Remote sensing based biophysical and predictive regression modeling approach have the potential for efficiently estimating soil moisture content over large areas. The study investigates the use of Moisture Stress Index (MSI) to estimate soil moisture variability in Alabama. In situ data were obtained from Soil Climate Analysis Network (SCAN) sites in Alabama and MSI developed from LANDSAT 8 OLI and LANDSAT 5 TM data. Pearson product moment correlation analysis showed that MSI strongly correlates with 16-day average growing season soil moisture measurements, with negative correlations of -0.519, -0.482 and -0.895 at 5, 10, and 20 cm soil depths respectively. The correlations of MSI and growing season moisture were low at sites where soil moisture was extremely low (<-0.3 at all depths). Simple linear regression model constructed for soil moisture at 20 cm depth (R²=0.79, p<0.05) correlated well with MSI values and was successfully used to estimate soil moisture percentage within a standard error of ± 3. Resulting MSI products were used to successfully produce the spatial distribution of soil moisture percentage at 20 cm depth. The study concludes that MSI is a good indicator of soil moisture conditions, and could be efficiently utilized in areas where in situ soil moisture data are unavailable.
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基于landsat的水分胁迫指数估算土壤水分百分比
全球农艺界需要快速和频繁地获得有关土壤水分变异和空间趋势的信息,以便最大限度地提高作物产量,以满足气候变化中不断增长的粮食需求。然而,原位土壤水分测量既昂贵又费力。基于遥感的生物物理和预测回归建模方法具有有效估算大面积土壤含水量的潜力。该研究调查了使用水分胁迫指数(MSI)来估计阿拉巴马州土壤水分的变化。原位数据来自阿拉巴马州的土壤气候分析网络(SCAN)站点和MSI站点,这些站点基于LANDSAT 8 OLI和LANDSAT 5 TM数据。Pearson积矩相关分析表明,MSI与16 d平均生长季土壤水分测量值呈强相关,在5、10和20 cm土壤深度分别为-0.519、-0.482和-0.895负相关。土壤湿度极低的样地(各深度均<-0.3),MSI与生长期水分的相关性较低。建立的20 cm深度土壤水分的简单线性回归模型(R²=0.79,p<0.05)与MSI值具有良好的相关性,并成功地用于估计土壤水分百分比,标准误差为±3。利用所得的MSI产品成功地获得了20 cm深度土壤水分百分比的空间分布。研究结果表明,MSI是土壤水分状况的良好指标,可以在缺乏原位土壤水分数据的地区有效利用。
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