Chuan Xiong;Liang Yuan;Zhenzhan Wang;Jiancheng Shi
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引用次数: 0
Abstract
The thermal infrared (TIR) emissivity and physical temperature of snow together determine the thermal radiation of snow. The modeling of snow and ice TIR emissivity is important for climate models and remote sensing. Previous snow and ice TIR emissivity models fail in predicting the sensitivity of emissivity to snow type and snow microstructure, which was measured in experiments. Empirical models were proposed to simulate such sensitivity but not in a unified theoretical framework. In this study, we propose a snow and ice TIR emissivity model based on photon tracking by assuming that the geometric optics approximation is still valid in TIR spectral region. It is proved that the proposed model can predict both the TIR emissivity’s sensitivity to grain size for small grain sizes and the TIR emissivity’s sensitivity to snow density. These features can fully explain the experiment observed features. Moreover, the proposed model simulates snow and ice TIR emissivity in a unified theoretical framework. We also explain that the observed emissivity’s sensitivity to snow type is actually caused by the sensitivity to snow density, not grain size. This proposed model can be further used in climate models and remote sensing.
雪的热红外辐射率和物理温度共同决定了雪的热辐射。冰雪热红外辐射率模型对气候模型和遥感非常重要。以往的冰雪 TIR 发射率模型无法预测发射率对雪类型和雪微观结构的敏感性,而这是在实验中测得的。有人提出了模拟这种敏感性的经验模型,但没有统一的理论框架。在本研究中,我们假设几何光学近似在 TIR 光谱区仍然有效,提出了基于光子跟踪的冰雪 TIR 发射率模型。研究证明,所提出的模型既能预测小粒径冰雪的近红外发射率对粒径的敏感性,也能预测近红外发射率对雪地密度的敏感性。这些特征可以完全解释实验观测到的特征。此外,所提出的模型在统一的理论框架下模拟了冰雪的红外发射率。我们还解释了观测到的发射率对雪类型的敏感性实际上是由对雪密度而不是粒度的敏感性引起的。该模型可进一步应用于气候模型和遥感领域。
期刊介绍:
IEEE Transactions on Geoscience and Remote Sensing (TGRS) is a monthly publication that focuses on the theory, concepts, and techniques of science and engineering as applied to sensing the land, oceans, atmosphere, and space; and the processing, interpretation, and dissemination of this information.