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Actual evapotranspiration estimation by means of airborne andsatellite remote sensing data

机译:通过空气传播遥感数据的实际蒸发估计

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During the last the two decades, the scientific community developed detailed mathematical models for simulating land surface energy fluxes and crop evapotranspiration rates by means of a energy balance approach. These models can be applied in large areas and with a spatial distributed approach using surface brightness temperature and some ancillary data retrieved from satellite/airborne remote sensed imagery. In this paper a district scale application in combination with multispectral (LandaSat 7 TMdata) and hyperspectral airborne MIVIS data has been carried out to test the potentialities of two different energy balance models to estimate evapotranspiration fluxes from a set of typical Mediterranean crops (wine, olive, citrus). The impact of different spatial and radiometric resolutions of MIVIS (3m x 3m) and LandSat (60m x 60m) on models-derived fluxes has been investigated to understand the roles and the main conceptual differences between the two models which respectively use a "single-layer" (SEBAL) and a "two-layer"(TS) schematisation.
机译:在过去的二十年中,科学界开发了通过能量平衡方法模拟陆地能量通量和作物蒸散率的详细数学模型。这些型号可以应用于大面积和使用表面亮度温度的空间分布式方法以及从卫星/空气遥控图像中检索的一些辅助数据。在本文中,已经进行了与多光谱(Landasat 7 TMDATA)和高光谱空气传播数据组合的地区规模应用,以测试两种不同能量平衡模型的潜力,以估算一套典型的地中海作物(葡萄酒,橄榄葡萄酒,柑橘类)。已经研究了不同空间和辐射分辨率的影响和辐射分辨率(3m x 3M)和Landsat(60m x 60m)对模型衍生的势态的影响,以了解两个模型之间的角色和主要概念差异,分别使用“单一 - 层“(SEBAL)和”两层“(TS)模板。

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