基于月球的吉林一号卫星在轨辐射定标研究

为了使吉林一号卫星遥感数据得到更好的应用,利用月球为辐射源对吉林一号光谱卫星进行了在轨绝对辐射定标研究,以对实验室定标系数进行改进。考虑到定标系数具有时效性,将观测数据按时间分组后定标,利用ROLO模型计算卫星观测时刻月球辐照度,构建ROLO模型值与卫星观测值之间的关系并进行最小二乘拟合,从而获得19个谱段的两组定标系数。最后,将定标结果与吉林一号场地定标、高分四号卫星和SeaWiFS月球观测数据进行对比验证。结果表明：对月定标结果稳定,两组定标系数线性拟合的不确定度分别为1.72%和1.24%;在光谱形状上,利用月球定标后月球光谱曲线平滑,光谱形状与月球辐射特性一致,与场地定标相比,各波段相对大小在定性上得到极大改善;在绝对辐射值上,定标结果与高分四号卫星月球辐照度平均相对误差为8.1%,与SeaWiFS两个波段的平均误差为0.90%和7.42%。本研究说明月球定标是卫星在轨辐射定标及真实性检验的有效途径。     

高光谱遥感地形影响建模与仿真

针对地形起伏对高光谱遥感图像几何变形和辐射变化的影响,建立高光谱遥感地形影响模型.该模型利用传感器位置、姿态和视场角建立模拟图像像元坐标和地面空间坐标之间的成像几何关系,利用地表反射率、数字高程模型等数据,考虑大气辐射传输过程,计算起伏地形下传感器入瞳辐亮度图像,并经过空间分辨率转换,生成最终遥感模拟图像,实现高光谱遥感地形影响精确建模.利用西藏驱龙地区Hyperion数据和其它相关数据进行仿真分析,将模拟图像和原始图像进行对比,结果比较吻合,表明该模型具有较好的模拟效果.     

利用6S进行月光条件下遥感器信号模拟研究

以太阳为光源的卫星遥感器,可以采用6S或MODTRAN等辐射传输计算软件对其入瞳处的辐亮度进行计算。而在微光或月光条件下,遥感器是对观测目标反射的月亮辐射进行遥感观测,因此在进行辐射传输计算时需要代入月球的辐照度数据。可以利用已公布的月球表面反射率和已知的大气层外太阳辐照度来计算月球辐照度,并对6S辐射传输计算进行适当的修改进行计算。通过对月球辐照度计算原理进行了详细的描述并计算得到了波长在0.250μm~1.500μm范围内的月球表面辐照度,并给出了一个宽波段遥感器的微光动态范围。     

覆盖我国的气象卫星系统及其应用

引言□□气象卫星自６０年代初问世以来，在此后的３０余年中得到了极大的发展。随着卫星和处理技术的不断进步，人类得以利用气象卫星从太空获取大量有关地球及其大气的物理和生态参数，使我们对地球的了解从深度到广度上都达到了前所未有的程度。我国是使用气象卫星资料较早的国家之一，早在１９６９年就已开始接收、处理和应用国外气象卫星的资料。同时，亦在积极地研制和发展我国自己的气象卫星系统。我国于１９８８年和１９９０年先后成功地发射了两颗自行研制的极轨气象卫星风云－１Ａ和１Ｂ（ＦＹ－１Ａ和１Ｂ），它们的后续星（ＦＹ…     

“高分五号”全谱段相机可展开定标漫反射板设计

为了对“高分五号”卫星全谱段光谱成像仪的太阳反射谱段辐射性进行长期监测与校正，并针对其谱段范围宽、精度要求高、口径大、使用寿命长等特点与要求，优化设计了可展开的漫反射板进行全光路全视场的辐射定标。定标漫反射板安装在相机光学系统的前端侧面，不影响相机正常成像，在定标时通过驱动机构展开漫反射板到相机前端，根据“高分五号”卫星轨道特点、定标能量要求及相机安装矩阵等设计定标漫反射板展开角度为39°。研制了430mm×430mm大尺寸聚四氟乙烯漫反射板组件以保证在展开时满足全光路全视场的定标，漫反射板在420～2400nm光谱范围内半球反射率高于95%，在相机观测方向BRDF变化优于25%。同时，设计了漫反射板稳定性监视辐射计用于监测漫反射板在轨性能衰减，监测精度15%。在轨定标精度分析为476%，满足指标要求。     

高层大气臭氧对于太阳紫外辐射27天波动的响应

本文利用Ｓｏｌａｒ Ｍｅｓｏｓｐｈｅｒｅ Ｅｘｐｌｏｒｅｒ（ＳＭＥ）卫星１９８２年和１９８３年太阳紫外辐射和赤道地区５０－９０ｋｍ臭氧分布的红外观测资料，对臭氧地太阳紫外辐射２７天振荡的响应进行了研究，并且利用大气光化波动模式对其进行了理论计算，计算结果与实测结果基本一致。     

FY-2卫星扫描辐射仪在轨定标方法

ＦＹ－ ２ 在轨定标是云图定量处理的关键。首先叙述了ＦＹ－ ２ 可见光、红外和水汽通道的定标方法;然后介绍了星上各通道的电定标及黑体定标的过程。结果表明红外通道在轨定标曲线与实验室定标非常接近。     

星载多光谱遥感器太阳定标技术的进展

星载多光谱遥感器的太阳定标器一般选择太阳作为基准光源 ,通过它将太阳辐射引入星载遥感器并调节到星载遥感器的动态范围内 ,对星载遥感器进行绝对辐射定标 ,也可对星载遥感器性能变化进行监测和校正。文章介绍一些最具代表性的星载多光谱遥感器的太阳定标器 ,并进行了分析 ,以反映太阳定标技术的现状与发展。目前采用太阳漫射器的星上定标方法可以实现全视场、全孔径、端点到端点的定标。这一方法的严重缺点是漫射器反射比随时间变化。为了解决这一问题 ,设计一种比辐射计或反射比标定装置来监测漫射器的辐亮度、反射比以及太阳常数。因此这种定标方法是很有前途的 ,在现代一些先进的星载多光谱遥感器上获得应用。通过对此方法的分析 ,提出了在太阳漫射器研制中的一些关键技术。     

风云一号卫星红外通道定标精度的检验

在气象卫星资料的定量应用中,定标是极为重要的。文章应用相对定标方法,对FY-1B 和NOAA 卫星的红外通道的定标精度进行了相对检验,结果表明两者之间的偏差不超过±1℃。     

基准星辐射定标的辐射传递链路研究

为进一步提高遥感信息定量化应用水平,提高在轨辐射定标精度和定标频次,提出一种基于基准星的全谱段、全口径在轨绝对辐射定标方法,方法适用于可见近红外谱段;定标传递中辐射基准可溯源至SI(国际单位)。通过比较现有定标方法和基准星辐射定标的优缺点,分析基准星辐射基准溯源特性,建立太阳 基准星 遥感器的辐射传递模型,以高分一号和高分二号卫星为例,其作为待定标遥感器,对基准星定标的约束条件进行仿真分析,得出基准星辐射传递不确定度为13%。仿真结果验证了基准星定标方法的可行性,对遥感器辐射定标精度、频次的进一步提高提供了依据。     

A comparison of atmospheric aerosol measurements by various satellite sensors

Investigations to measure the vertical optical thickness of aerosols over ocean surfaces has been conducted using several different satellite sensors. Landsat 1 and Landsat 2 data originally confirmed that a linear relationship exists between the upwelling visible radiance and the aerosol optical thickness (about 90% of this thickness is generally in the lowest 3 km of the atmosphere). Similar relationships have also been found for sensors on GOES-1, SMS-2, NOAA-5, and NOAA-6 satellites. The linear relationship has been shown theoretically to vary with the aerosol properties, such as size distribution and refractive index, although the Landsat data obtained at San Diego showed little variability in the relationship. The differences between the results found for the various satellite sensors are discussed, and are attributed mainly to uncertainties in the calibration of the sensors. To investigate the general applicability of the technique to different locations, a global-scale ground truth experiment was conducted with the AVHRR sensor on NOAA-6 to determine the relationship at eleven ocean sites around the globe. Analysis of the data shows good agreement between the satellite and ground truth values of the aerosol optical thickness, and indicates that the technique has global application. At two of the sites, multispectral radiometric measurements of the Junge aerosol size distribution parameter were made, and showed good agreement with a value inferred from the AVHRR Channels 1 and 2 radiances.     

FY-2卫星的空间环境数据接收及警报系统

介绍了FY—2卫星探测数据的流通过程及接收处理．首先在FY-2卫星及探测器系统中，环境探测数据被收集、调制并发射，再由地基数据接收及解调系统将数据信号放大、解调还原并发送，最后由数据处理及警报系统将数据接收处理、保存显示，并对太阳质子事件、x耀斑进行自动电话报警．该系统是保障航天器安全和提高抗辐照水平的重要手段．     

A novel method for destriping of OCM-2 data and radiometric performance analysis for improved ocean color data products

Despite the capability of Ocean Color Monitor aboard Oceansat-2 satellite to provide frequent, high-spatial resolution, visible and near-infrared images for scientific research on coastal zones and climate data records over the global ocean, the generation of science quality ocean color products from OCM-2 data has been hampered by serious vertical striping artifacts and poor calibration of detectors. These along-track stripes are the results of variations in the relative response of the individual detectors of the OCM-2 CCD array. The random unsystematic stripes and bandings on the scene edges affect both visual interpretation and radiometric integrity of remotely sensed data, contribute to confusion in the aerosol correction process, and multiply and propagate into higher level ocean color products generated by atmospheric correction and bio-optical algorithms. Despite a number of destriping algorithms reported in the literature, complete removal of stripes without residual effects and signal distortion in both low- and high-level products is still challenging. Here, a new operational algorithm has been developed that employs an inverted gaussian function to estimate error fraction parameters, which are uncorrelated and vary in spatial, spectral and temporal domains. The algorithm is tested on a large number of OCM-2 scenes from Arabian Sea and Bay of Bengal waters contaminated with severe stripes. The destriping effectiveness of this approach is then evaluated by means of various qualitative and quantitative analyses, and by comparison with the results of the previously reported method. Clearly, the present method is more effective in terms of removing the stripe noise while preserving the radiometric integrity of the destriped OCM-2 data. Furthermore, a preliminary time-dependent calibration of the OCM-2 sensor is performed with several match-up in-situ data to evaluate its radiometric performance for ocean color applications. OCM-2 derived water-leaving radiance products obtained after calibration show a good consistency with in-situ and MODIS-Aqua observations, with errors less than the validated uncertainties of ±5% and ±35% endorsed for the remote-sensing measurements of water-leaving radiance and retrieval of chlorophyll concentrations respectively. The calibration results show a declining trend in detector sensitivity of the OCM-2 sensor, with a maximum effect in the shortwave spectrum, which provides evidence of sensor degradation and its profound effect on the striping artifacts in the OCM-2 data products.     

FY-3 Meteorological Satellites and the Applications

FY-3 is the second generation polar-orbiting meteorological satellite of China. The first satellite named FY-3A of this series was launched on 27 May 2008. The first operational satellite named FY-3C of this series was launched on 23 September, 2013. The new generation satellites are to provide three-dimensional, quantitative, multi-spectral global remote sensing data under all weather conditions, which will greatly help the operational numerical weather prediction, global climate change research, climate diagnostics and prediction, and natural disaster monitoring. They will also provide help for many other fields such as agriculture, forestry, oceanography and hydrology. With the abovementioned capability, the FY-3 satellites can make valuable contributions to improving weather forecasts, global natural-disaster and environmental monitoring.      

Vegetation health: Nature's climate monitor

Observational data to effectively evaluate weather effects, which accumulate into current climate status, are available for affluent nations but often are inadequate elsewhere. Data acquired by satellite sensors in the visible-near infrared portion of the reflected solar energy spectrum have been accumulated daily since 1965 and for the earth's emitted radiance in the 11000 nm window since 1972. With the advent of the TIROS-N satellite in 1978, the solar reflected energy has been sensed in two separate channels and beginning with NOAA-6, the second vehicle of the TIROS-N family, these two channels became complementary rather than overlapping. This feature makes vegetative monitoring possible and now is being exploited to provide daily experimental products. These global vegetative index (GVI) arrays have been used to observe and map the effects of droughts, floods, adverse winds and thermal stresses on the global arable lands. These data and the related sea surface temperatures, both derived from satellite data, provide realistic measures of the global climate and can assist climatic forecasting.     

空间TDICCD相机动态信噪比计算方法研究

信噪比是空间光学相机系统的主要设计指标之一,可用于表征相机的辐射性能。文章通过建立遥感卫星轨道模型,分析计算一年中任意时刻用太阳高度角和卫星观测角描述太阳、卫星、地面目标点之间的相对位置关系,并将计算得到的卫星观测角和太阳高度角等参数导入大气传输软件MODTRAN,输出在相机入瞳处的地面目标光谱辐亮度,再根据信噪比的计算方法,最后完成TDICCD相机动态的信噪比计算值。通过该方法,可以计算任一时刻任一观测目标的信噪比,这将有利于判断在某一时刻的能量是否满足观测要求,以随时改变TDICCD的探测器级数,使得成像像质达到最佳。