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首页> 外文期刊>International journal of remote sensing >Mapping soil moisture in the central Ebro river valley (northeast Spain) with Landsat and NOAA satellite imagery: a comparison with meteorological data
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Mapping soil moisture in the central Ebro river valley (northeast Spain) with Landsat and NOAA satellite imagery: a comparison with meteorological data

机译:利用Landsat和NOAA卫星图像绘制埃布罗河中部山谷(西班牙东北部)的土壤湿度:与气象数据的比较

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This paper analyses and maps the spatial distribution of soil moisture using remote sensing: National Oceanic and Atmospheric Administration (NOAA) Advanced Very High Resolution Radiometer (AVHRR) and Landsat-Enhanced Thematic Mapper (ETM + ) images. The study was carried out in the central Ebro river valley (northeast Spain), and examines the spatial relationships between the distribution of soil moisture and several meteorological and geographical variables following a long, intense dry period (winter 2000). Soil moisture estimates were obtained using thermal, visible and near-infrared data and by applying the 'triangle method', which describes relationships between surface temperature (T_s) and fractional vegetation cover (F_r). Low differences were found between the soil moisture estimates obtained using AVHRR and ETM + sensors. Soil moisture estimated using remote sensing is close to estimations obtained from climate indices. This fact, and the high similarity between estimations of both sensors, suggests the reasonable reliability of soil moisture remote sensing estimations. Moreover, in estimations from both sensors the spatial distribution of soil moisture was largely accounted for by meteorological variables, mainly precipitation in the dry period. The results indicate the high reliability of remote sensing for determining areas affected by water deficits and for quantifying drought intensity.
机译:本文使用遥感技术分析并绘制了土壤水分的空间分布图:美国国家海洋和大气管理局(NOAA)先进的超高分辨率辐射计(AVHRR)和Landsat增强型专题测绘仪(ETM +)图像。这项研究是在埃布罗河中部山谷(西班牙东北部)进行的,研究了长期干旱后(2000年冬季)土壤水分的分布与若干气象和地理变量之间的空间关系。利用热,可见和近红外数据并应用“三角法”获得土壤湿度估算值,该方法描述了地表温度(T_s)和植被覆盖率(F_r)之间的关系。发现使用AVHRR和ETM +传感器获得的土壤湿度估算值之间差异很小。使用遥感估算的土壤水分接近于根据气候指数获得的估算。这一事实以及两个传感器的估算值之间的高度相似性表明土壤湿度遥感估算值具有合理的可靠性。此外,在两个传感器的估算中,土壤湿度的空间分布在很大程度上是由气象变量引起的,主要是干旱时期的降水。结果表明,遥感技术在确定受缺水影响的地区和定量干旱强度方面具有很高的可靠性。

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