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首页> 外文期刊>Remote Sensing of Environment: An Interdisciplinary Journal >A review of earth surface thermal radiation directionality observing and modeling: Historical development, current status and perspectives
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A review of earth surface thermal radiation directionality observing and modeling: Historical development, current status and perspectives

机译:地球表面热辐射方向性观察和建模综述:历史发展,当前地位和观点

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The Earth surface thermal infrared (TIR) radiation shows conspicuously an anisotropic behavior just like the bidirectional reflectance of visible and near infrared spectral domains. The importance of thermal radiation directionality (TRD) is being more and more widely recognized in the applications because of the magnitude of the effects generated. The effects of TRD were originally evidenced through experiments in 1962, showing that two sensors simultaneously measuring temperature of the same scene may get significantly different values when the viewing geometry is different. Such effect limits inter-comparison of measurement datasets and land surface temperature (LST) products acquired at different view angles, while raising the question of measurement reliability when used to characterize land surface processes. These early experiments fostered the development of modeling approaches to quantify TRD with the aim of developing a correction for Earth surface TIR radiation. Initiatives for pushing the analysis of TIR data through modeling have been lasted since 1970s. They were initially aimed at mimicking the observed TIR radiance with consideration of canopy structure, component emissivities and temperatures, and Earth surface energy exchange processes. Presently, observing the Earth surface TRD effect is still a challenging task because the TIR status changes rapidly. Firstly, a brief theoretical background and the basic radiative transfer equation are presented. Then, this paper reviews the historical development and current status of observing TRD in the laboratory, in-situ, from airborne and space-borne platforms. Accordingly, the TRD model development, including radiative transfer models, geometric models, hybrid models, 3D models, and parametric models are reviewed for surfaces of water, ice and sea, snow, barren lands, vegetation and urban landscapes, respectively. Next, we introduce three potential applications, including normalizing the LST products, estim
机译:地球表面热红外线(TIR)辐射显着地显示出各向异性行为,就像是可见和近红外光谱畴的双向反射率。由于产生的效果的大小,热辐射方向性(TRD)的重要性在应用中越来越广泛地识别。 TRD的效果最初通过1962年的实验证明,表示观察几何形状不同的同时测量相同场景温度的两个传感器可以显着不同。这种效果限制了在不同视角获取的测量数据集和陆表面温度(LST)产品的相互比较,同时在用于表征陆地过程时提高测量可靠性问题。这些早期的实验促进了建模方法的发展,以量化TRD的目的,目的是开发地面表面TIR辐射的校正。自20世纪70年代以来,通过建模推动TIR数据分析的倡议。最初旨在考虑到冠层结构,组分发射率和温度和地球表面能量交换过程来模仿观察到的TIR亮。目前,观察地球表面TRD效果仍然是一个具有挑战性的任务,因为TIR状态迅速变化。首先,提出了简要的理论背景和基本的辐射转移方程。然后,本文审查了实验室,原位从空中和太空平台观察TRD的历史发展和现状。因此,对于水,冰和海,雪,荒芜土地,植被和城市景观的表面,对包括辐射传输模型,几何模型,混合模型,3D模型和参数模型进行了综述。接下来,我们介绍了三种潜在的应用,包括标准化LST产品,估计

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