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Thermal infrared imagery from the Geoscan Mk II scanner and its calibration: two case histories from Nevada--Ludwig Skarn (Yerington District) Virginia City

机译:Geoscan Mk II扫描仪的红外热成像及其校准:内华达州的两个案例历史-路德维希·斯卡恩(Yerington District)和弗吉尼亚市

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Abstract: The 24-channel Geoscan scanner includes six grating-dispersed thermal infrared channels, co- registered with the 18 VNIR and SWIR bands. Considerable silicate (hydroxyl) discrimination can be seen in the SWIR band images but will not be treated further in this paper. Each of the TIR bands has a bandpass of 530 nm, centered between 8.64 and 11.28 $mu@m band centers dispersed onto a linear detector array of HgCdTe. The system has been flown over Ludwig, Nevada three times (May 1989/June 1990), and twice over Virginia City, Nevada (June 1989/Aug. 1990). Pixel sizes ranged from 3 m to 6 m in this 'research-mode' flying. In flight the scanner is operated in a noncalibrated, relative-radiance mode in all of the 24 channels. A sample of the terrain to be mapped is overflown, during which the offsets of each channel are set to mid-range (DN $EQ 127), with the data spread by the gain setting so as to occupy all of the 8-bit range. The recording therefore is of the 8 bits of data spread about the average (relative) brightness of the terrain in that band. In this manner, this scanner differs from almost every other unit either in airborne use or in the Landsat satellites. These units record absolute brightness from which, by use of the calibration parameters, the absolute radiance of the terrain may be reconstructed. The problem is to perform a transformation of the imagery to apparent reflectance allow comparison of the spectra extracted from the airborne imagery to ground-measured spectra. TIR spectra have also been obtained in ground-based stationary laboratory-type operation of the aircraft scanner, viewing warm samples (heated by the sun to about 45 C) for fifteen of the major rock-type assemblages. These laboratory-scanner match the airborne-scanner spectra abstracted from the imagery data as well as direct exitance spectra obtained previously from other sun-warmed samples.!
机译:摘要:24通道Geoscan扫描仪包括6个光栅分散的热红外通道,与18个VNIR和SWIR波段共同记录。在SWIR波段图像中可以看到相当多的硅酸盐(羟基)区分度,但本文将不作进一步处理。每个TIR波段具有530 nm的带通,中心在8.64和11.28μm波段中心,分散在HgCdTe线性检测器阵列上。该系统已经在内华达州路德维希上空飞行了三次(1989年5月/ 1990年6月),并在内华达州弗吉尼亚市上空飞行了两次(1989年6月/ 1990年8月)。在这种“研究模式”飞行中,像素大小从3 m到6 m不等。在飞行中,扫描仪在所有24个通道中均以非校准的相对辐射度模式运行。溢出了要映射的地形的样本,在此期间,每个通道的偏移设置为中间范围(DN $ EQ 127),数据通过增益设置扩展,从而占据了所有8位范围。因此,记录是围绕该频带中地形的平均(相对)亮度分布的8位数据。以此方式,该扫描仪在机载使用或Landsat卫星上几乎与其他所有单元都不相同。这些单位记录绝对亮度,通过使用校准参数,可以从中重建地形的绝对辐射度。问题在于如何将图像转换为表观反射率,从而可以比较从机载图像提取的光谱与地面测量的光谱。在飞机扫描仪的地面固定式实验室型操作中,还通过观察十五种主要岩石类型组合的热样本(被太阳加热至约45 C),获得了TIR光谱。这些实验室扫描仪与从图像数据中提取的机载扫描仪光谱以及先前从其他日晒样品获得的直接出射光谱相匹配!

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