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Soil moisture variability across different scales in an Indian watershed for satellite soil moisture product validation

机译:印度流域卫星土壤水分产品验证的不同尺度土壤水分变异性

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Strategic ground-based sampling of soil moisture across multiple scales is necessary to validate remotely sensed quantities such as NASA's Soil Moisture Active Passive (SMAP) product. In the present study, in-situ soil moisture data were collected at two nested scale extents (0.5 km and 3 km) to understand the trend of soil moisture variability across these scales. This ground-based soil moisture sampling was conducted in the 500 km~2 Rana watershed situated in eastern India. The study area is characterized as sub-humid, sub-tropical climate with average annual rainfall of about 1456 mm. Three 3×3 km square grids were sampled intensively once a day at 49 locations each, at a spacing of 0.5 km. These intensive sampling locations were selected on the basis of different topography, soil properties and vegetation characteristics. In addition, measurements were also made at 9 locations around each intensive sampling grid at 3 km spacing to cover a 9×9 km square grid. Intensive fine scale soil moisture sampling as well as coarser scale samplings were made using both impedance probes and gravimetric analyses in the study watershed. The ground-based soil moisture samplings were conducted during the day, concurrent with the SMAP descending overpass. Analysis of soil moisture spatial variability in terms of areal mean soil moisture and the statistics of higher-order moments, i.e., the standard deviation, and the coefficient of variation are presented. Results showed that the standard deviation and coefficient of variation of measured soil moisture decreased with extent scale by increasing mean soil moisture.
机译:跨多种尺度的土壤水分的战略地面采样是必要的,以验证遥感量,如美国国家航空航天局的土壤湿度活性无源(SMAP)产品。在本研究中,原位土壤水分数据在两个嵌套秤范围(0.5 km和3公里),以了解这些尺度的土壤湿度变异性的趋势。该基于地面的土壤水分抽样是在印度东部的500公里〜2个Rana流域进行。该研究区的特点是潜水,亚热带气候,平均年降雨量约为1456毫米。每天49个地点在49个地点举行三个3×3km方形网格,间距为0.5公里。这些密集型采样位置是在不同的地形,土壤性质和植被特征的基础上选择的。此外,还在每次密集采样网格周围的9个位置进行测量,以3km间距覆盖9×9km方形网格。使用研究流域中的阻抗探针和重量分析,在研究流域中进行了强化细尺土壤水分抽样以及较粗糙的尺度样品。白天进行地面土壤水分采样,并发与下坡立交桥同时进行。介绍了地区均值土壤水分的土壤水分空间变异性分析及高阶矩的统计,即标准偏差和变异系数。结果表明,通过增加平均土壤水分,测量土壤水分的标准偏差和测量土壤水分的变异系数随着均值的土壤水分而降低。

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