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Angular variation of thermal infrared emissivity for some natural surfaces from experimental measurements

机译:根据实验测量,某些自然表面的热红外发射率的角度变化

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摘要

Multiangle algorithms for estimating sea and land surface temperature with Along-Track Scanning Radiometer data require a precise knowledge of the angular variation of surface emissivity in the thermal infrared. Currently, few measurements of this variation exist. Here an experimental investigation of the angular variation of the infrared emissivity in the thermal infrared (8-14-μm) band of some representative samples was made at angles of 0°-65° (at 5° increments) to the surface normal. The results show a decrease of the emissivity with increasing viewing angle, with water showing the highest angular dependence (~7% from 0° to 65° views). Clay, sand, slime, and gravel show variations of approximately 1-3% for the same range of views, whereas a homogeneous grass cover does not show angular dependence. Finally, we include an evaluation of the impact that these data can produce on the algorithms for determining land and sea surface temperature from double-angle viewe.
机译:使用“沿航迹扫描辐射计”数据估算海洋和陆地表面温度的多角度算法需要对热红外中表面发射率的角度变化有精确的了解。当前,很少有这种变化的度量。在此,对一些代表性样品在相对于表面法线的角度为0°-65°(以5°递增)的情况下,对热红外(8-14-μm)波段中红外发射率的角度变化进行了实验研究。结果表明,发射率随视角的增加而降低,水显示出最大的角度依赖性(从0°到65°视角约为7%)。在相同的视野范围内,粘土,沙子,煤泥和砾石的变化约为1-3%,而均匀的草皮则没有角度依赖性。最后,我们评估了这些数据可能对从双视角确定陆地和海洋表面温度的算法产生的影响。

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