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ESTIMATION OF LAND SURFACE ENERGY FLUXES: AN APPLICATION OF SATELLITE REMOTE SENSING PROCEDURE

机译:土地表面能量通量估算:卫星遥感程序的应用

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Surface energy fluxes, including sensible heat, latent heat, net radiation, and soil heat flux, playcrucial role in surface energy dynamics of any terrain or landscapes. Estimation or measurement ofthese energy fluxes is critical for completing the water balance in terrestrial ecosystems, and thereforeaccurately predicting the effects of global climate and land use change. There are various methodsavailable for ET estimation. Bowen ratio energy balance and eddy correlation techniques offerpowerful alternatives for measuring land surface energy fluxes. In spite of the elegance, high accuracyand theoretical attractions of these techniques for measuring ET, their practical use over large areascan be limited. These techniques provide measurements at a point scale and may not be practicalwhen quantifying water use over large areas due to the number of measurement sites needed and theoperational expense of such a dense network. Application of ET mapping from satellite measurementscan overcome aforementioned limitations. The objective of this study is to assess the performance ofthe METRICtm (Mapping Evapotranspiration at high Resolution using Internalized Calibration) modelfor estimating land surface energy fluxes to improve our understanding of processes that govern wateruse in managed and native ecosystems in south-central Nebraska.
机译:表面能通量,包括显热,潜热,净辐射和土壤热通量 在任何地形或景观的表面能动力学中都起着至关重要的作用。估计或测量 这些能量通量对于完成陆地生态系统中的水平衡至关重要,因此 准确预测全球气候和土地利用变化的影响。有各种各样的方法 可用于ET估算。鲍恩比能量平衡和涡流相关技术提供 用于测量陆地表面能量通量的强大替代方案。尽管优雅,但准确性高 和这些技术用于测量ET的理论吸引力,它们在大面积上的实际使用 可以限制。这些技术可提供以磅为单位的测量结果,可能不实际 由于所需的测量地点数量众多,并且在大面积上对用水进行量化时, 如此密集的网络的运营费用。 ET测量在卫星测量中的应用 可以克服上述限制。这项研究的目的是评估 METRICtm(使用内标法以高分辨率映射蒸散)模型 估计地表能量通量,以增进我们对控制水的过程的理解 在内布拉斯加州中南部的受管理和原生生态系统中使用。

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