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Estimation of actual evapotranspiration of Mediterranean perennial crops by means of remote-sensing based surface energy balance models

机译:基于遥感的地表能量平衡模型估算地中海多年生作物的实际蒸散量

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摘要

Actual evapotranspiration from typical Mediterranean crops has been assessed in a Sicilian study area by using surface energy balance (SEB) and soil-water balance models. Both modelling approaches use remotely sensed data to estimate evapotranspiration fluxes in a spatially distributed way. The first approach exploits visible (VIS), nearinfrared (NIR) and thermal (TIR) observations to solve the surface energy balance equation whereas the soil-water balance model uses only VIS-NIR data to detect the spatial variability of crop parameters. Considering that the study area is characterized by typical spatially sparse Mediterranean vegetation, i.e. olive, citrus and vineyards, alternating bare soil and canopy, we focused the attention on the main conceptual differences between one-source and two-sources energy balance models. Two different models have been tested: the widely used one-source SEBAL model, where soil and vegetation are considered as the sole source (mostly appropriate in the case of uniform vegetation coverage) and the two sources TSEB model, where soil and vegetation components of the surface energy balance are treated separately. Actual evapotranspiration estimates by means of the two surface energy balance models have been compared vs. the outputs of the agro-hydrological SWAP model, which was applied in a spatially distributed way to simulate one-dimensional water flow in the soil-plant-atmosphere continuum. Remote sensing data in the VIS and NIR spectral ranges have been used to infer spatially distributed vegetation parameters needed to set up the upper boundary condition of SWAP. Actual evapotranspiration values obtained from the application of the soil water balance model SWAP have been considered as the reference to be used for energy balance models accuracy assessment. Airborne hyperspectral data acquired during a NERC (Natural Environment Research Council, UK) campaign in 2005 have been used. The results of this investigation seem to prove a slightly better agreement between SWAP and TSEB for some fields of the study area. Further investigations are programmed in order to confirm these indications.
机译:通过使用表面能平衡(SEB)和土壤水平衡模型,在西西里研究区评估了典型地中海作物的实际蒸散量。两种建模方法都使用遥感数据以空间分布的方式估算蒸散通量。第一种方法利用可见(VIS),近红外(NIR)和热(TIR)观测来解决表面能平衡方程,而土壤-水平衡模型仅使用VIS-NIR数据来检测作物参数的空间变异性。考虑到研究区域的特征是典型的空间稀疏的地中海植被,即橄榄,柑橘和葡萄园,裸露的土壤和冠层交替,我们将注意力集中在一源和两源能量平衡模型之间的主要概念差异上。测试了两种不同的模型:广泛使用的单源SEBAL模型,其中土壤和植被被视为唯一的源(最适合在均匀植被覆盖的情况下使用)和两种源TSEB模型,其中土壤和植被组成为表面能平衡要分开处理。比较了通过两个表面能平衡模型估算的实际蒸散量与农业水文SWAP模型的输出量,该模型以空间分布方式应用于模拟土壤-植物-大气连续体中的一维水流。 VIS和NIR光谱范围内的遥感数据已被用于推断建立SWAP上限条件所需的空间分布植被参数。从土壤水分平衡模型SWAP的应用获得的实际蒸散量已被视为可用于能量平衡模型准确性评估的参考。使用了在2005年NERC(英国自然环境研究委员会)活动中获得的机载高光谱数据。这项研究的结果似乎证明SWAP和TSEB在研究区域的某些领域之间有更好的一致性。为了确定这些指示,需要进行进一步的研究。

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