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Airborne sampling of the reflectivity by the hyperspectral line scanner in a visible and near infrared wavelengths

机译:高光谱线扫描仪在可见和近红外波长的空中采样反射率

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Hyperspectral remote sensing is and was the focus of attention of the EARSeL. In the paper we present use of the novel type V9 (ImSpector) of the hyperspectral line scanner (HSLS) in visible and near infrared wavelengths aimed to sample reflectivity of the ground surface by airborne remote sensing. The airborne system was developed for the aerial sampling of hyper spectral data, while the platform was the helicopter Bell-206. The system was used in 2003 and first data were collected above minefields and suspected areas in two regions that have very different terrain characteristics, climate and other factors. Spectral resolution of the used HSLS V9 is up to 100 channels in the wavelengths from 430 nm to 900 nm, while the spatial resolution is determined by focal length of the optical objective, dimensions of the chip, width of the slit and distance h to the ground. The HSLS collects up to 24 spectral samples per second in a form of a gray level image. This image shows intensity of the reflected waves, and pixels at the right side of the image contain information about incident waves, collected by diffuse collector. Ratio of reflected and incident value at the wavelengthλ_i is coefficient of reflection at this wavelength. Waves reflected by ground surface are collected at nadir, by optical objective, incident waves are collected by diffuse collector oriented to the Sun. HSLS measures at height h above ground, this produces difficulties to the radiometric calibration. The values E_(inc) and E_(refl) measured by HSLS enable calculation of the reflection coefficient r according to the relation r = [G_(refl)E_(refl)/F(α)]/[G_(inc)E_(inc)/F(θ)]. While the gains of the channels G_(refl) and G_(inc) were not determined yet, instead of coefficient of reflection r, obtained value is measure of reflectivity r(G_(inc)/G_(refl)) and has maximum values greater than one. While for navigation of helicopter Bell-206 was not available inertial measuring unit, and for this purpose was used GPS and moving map with pilot in the loop, the spatial accuracy of hyper spectral samples is mainly limited by the accuracy of GPS data and undesired movements of the platform (heading, pitch, yaw). The common effect of the undesired variation ΔW of the width of the strip and of its displacement dy, can be conservatively estimated by max (|ΔW| + |dy|) < 0.1 W, W is width of the line sample. By use of described system were collected hyperspectral samples of the reflectivity above the minefields together with digital images in visible and near infrared wavelengths. Radiometric calibration and increase of spatial accuracy by use of inertial navigation measuring system will be realized in next phase of the system development.
机译:高光谱遥感是并且是耳塞的注意力。在本文中,我们在可见的和近红外波长中使用高光谱线扫描仪(HSL)的新型V9(IMSpector)的使用,其目的是通过空气传播遥感来对地面的反射率进行采样。为空中采样的超频数据开发了空气传播系统,而平台是直升机贝尔-206。该系统于2003年使用,并在雷区上方收集了第一数据,并在两个地区的疑似区域,具有非常不同的地形特征,气候和其他因素。使用的HSLS V9的光谱分辨率在430nm至900nm的波长中最多100个通道,而空间分辨率由光学物镜的焦距,芯片的尺寸,狭缝的宽度和距离H确定地面。 HSL在灰度级图像的形式下每秒收集最多24个光谱样本。该图像示出了反射波的强度,并且图像右侧的像素包含由漫射收集器收集的入射波的信息。波长λ_i的反射和入射值的比率是该波长的反射系数。由地面反射的波在Nadir上收集,通过光学物镜,通过漫射到太阳的漫射收集器收集入射波。 HSLS在地面高度H处测量,这会产生辐射校准的困难。由HSLS测量的值E_(INC)和E_(REVE)使得根据关系R = [G_(RETH)E_(RECT)/ F(α)] / [G_(INC)E_( inc)/ f(θ)]。虽然尚未确定通道G_(ROFT)和G_(INC)的增益,而不是反射系数R,所以获得的值是反射率R的测量(G_(INC)/ G_(RECH)),并且具有更大的值而不是一个。对于直升机贝尔-206的导航而不是可用的惯性测量单元,而对于此目的,使用GPS和循环中的飞行员移动地图,超频样本的空间精度主要受GPS数据和不希望的运动的准确性的限制平台(标题,俯仰,偏航)。通过最大(ΔW| + |)<0.1W,W是线样品的宽度,可以保守估计条带和其位移Dy的宽度的不希望变化ΔW的常见效果。通过使用所描述的系统,将雷区上方的反射率的高光谱样本与可见和近红外波长的数字图像一起。通过使用惯性导航测量系统,将在下一个阶段实现通过使用惯性导航测量系统的辐射校准和增加空间精度。

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