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遥感影像受大气的吸收散射以及地形起伏变化的影响,使得传感器接收到的辐射信号既包含了地物的信息,同时也包含了大气以及地形的信息。为了提高地表反射率的反演精度,需要去除遥感影像中大气和地形的影响。提出了一种基于查找表的Landsat8-OLI遥感影像的大气校正方法,该方法由6S辐射传输模型生成查找表,其中输入的参数包括大气水蒸汽含量、臭氧浓度和气溶胶光学厚度等MODIS大气参数产品。利用传统方法建立的大气参数查找表通常只考虑一部分因素,这对于以MODIS产品为输入参数的大气校正是不适用的。本文建立了一个包括大部分输入参数的高维大气校正查找表,对于Landsat-8 OLI传感器具有很高的通用性,通过进行光谱分析、与USGS地表反射率产品交叉验证等方式来验证模型的精度。验证结果表明该方法能有效地反演精确可靠的地表反射率。最后,采用目视解译、统计分析将校正结果与SEVI做对比分析,比较地形影响消减的效果。结果表明该模型与SEVI在地形消减的效果上作用相当。 相似文献
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《遥感技术与应用》2019,(5)
遥感影像受大气的吸收散射以及地形起伏变化的影响,使得传感器接收到的辐射信号既包含了地物的信息,同时也包含了大气以及地形的信息。为了提高地表反射率的反演精度,需要去除遥感影像中大气和地形的影响。提出了一种基于查找表的Landsat8-OLI遥感影像的大气校正方法,该方法由6S辐射传输模型生成查找表,其中输入的参数包括大气水蒸汽含量、臭氧浓度和气溶胶光学厚度等MODIS大气参数产品。利用传统方法建立的大气参数查找表通常只考虑一部分因素,这对于以MODIS产品为输入参数的大气校正是不适用的。本文建立了一个包括大部分输入参数的高维大气校正查找表,对于Landsat-8 OLI传感器具有很高的通用性,通过进行光谱分析、与USGS地表反射率产品交叉验证等方式来验证模型的精度。验证结果表明该方法能有效地反演精确可靠的地表反射率。最后,采用目视解译、统计分析将校正结果与SEVI做对比分析,比较地形影响消减的效果。结果表明该模型与SEVI在地形消减的效果上作用相当。 相似文献
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介绍了利用交互式数据语言(Interactive Data Language,IDL)开发TM/ETM遥感影像大气与地形校正模型的详细过程,以2000年4月30日密云ETM影像为例,对大气与地形校正方法的有效性和实用性进行了验证。结果表明,该方法有效地消除了大气与地形影响,提高了地表反射率等地表参数的反演精度和数据质量,为进一步开展定量遥感研究提供了数据质量保障。 相似文献
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针对高光谱数据大气校正耗时长和查找表构建不准确等问题,提出基于MODTRAN辐射传输模型实时创建大气校正参数查找表的方法,并应用于水体叶绿素浓度反演。首先,基于高光谱数据实时构建大气校正参数查找表;其次,根据循环迭代反演得到水汽含量和气溶胶光学厚度对查找表插值得到各个波段的大气校正参数,从而完成所有波段数据的大气校正;最后,选择植被、土壤和水体3类典型地物精度分析,并基于反演水体的叶绿素a浓度验证大气校正精度的可靠性。实验结果表明:该方法明显优于6S、FLAASH等大气校正方法;在运行效率上,在多线程并行加速后,运行效率提升了2~4倍;基于水体反射率数据反演水体叶绿素a浓度,反演模型预测集验证中ρ为0.804 7,RMSE为1.8。 相似文献
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山地TM遥感影像大气辐射校正模型改进及地表反射率反演 总被引:3,自引:0,他引:3
基于光学遥感辐射传输理论,着重阐述了地形对天空散射光相互作用及邻近像元的影响,提出了一种改进的山地大气辐射校正模型及地表反射率反演方法;基于IDL编程实现模型算法,选择贵州黎平县丘陵森林覆盖典型研究区,结合Landsat-5TM和1∶50000DEM数据进行了实例验证、评价与分析。研究结果表明,本研究方法能够同时有效消除TM数据的大气与地形影响,提高地表反射率反演精度与数据质量,将进一步推动山地光学遥感数据的定量分析与应用。 相似文献
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遥感影像地形和大气校正是提高定量化遥感数据处理精度的重要因素。目前的数据处理软件系统集成了一些地形和大气校正算法,但在应用中还存在不能获取重要的地形参数(如阴影因子、天空可视因子等),需提供精准DEM和校正方法基于朗伯体地表假设等问题。为应对遥感专业用户需求,设计并实现了遥感影像地形与大气校正软件系统,用以对影像进行地形辐射校正、获取DEM数据和相关地形参数、地形与大气校正等。介绍了系统的功能模块设计并展示了系统的原型版本,并应用系统中的地形和大气校正方法获取了HJ/CCD影像和Landsat/TM影像的反射率。校正结果表明:该系统中的BRDF模型能够有效消除地形影响。系统的实现可以为遥感科学研究和应用提供支撑。 相似文献
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ETM+数据绝对反射率反演方法分析 总被引:12,自引:2,他引:12
将传感器原始记录信号反演为地面反射率对于遥感定量化应用非常重要。为了寻找一种简单、精度高的绝对反射率反演方法,本文以新疆哈密为试验区,使用经验线方法和基于模拟大气状况的辐射传输模型方法对1999年8月的ETM 数据进行了反演研究。通过将各反演方法得到的反射率值与地面实测值及星上反射率进行对比来验证反演效果,发现经验线方法精度最高,中误差仅为0.063,而基于模拟大气状况的辐射传输模型方法精度差,甚至不如未经大气校正的数据。这是由于星上定标系数误差、辐射传输方程自身误差以及模拟大气误差综合的结果,本研究也说明今后在使用辐射传输模型进行大气校正时要慎重考虑。 相似文献
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卫星遥感影像数据的地形影响校正 总被引:6,自引:2,他引:6
地形影响校正是遥感影像辐射校正的主要内容,是获得地表真实反射率的必不可少的一步。本文提出的方法中,将6S大气校正模型与数字高程模型(DEM)结合起来,计算出水平地面上接收到的直接辐射与漫射辐射,并采用一个简单公式将其转化到地形坡面上,从而实现了对地面的辐射能量校正,同时,6S模型对卫片还进行了大气改正,可输出卫片在大气层底部的辐射亮度与反射率;然后将基于坡面的反射率换算到其在水平面上的对应值,即实现了对反射率的地形影响校正。在我们所实施的“滇金丝猴保护项目”的植被研究中,应用本方法对梅里雪山区域的ETM+影像进行了校正,大大减小了地形对遥感数据的附加影响。 相似文献
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为了消除影像中的大气影响,反演地表真实反射率,需要进行大气校正。6S是通用的大气校正模型之一,但是对于覆盖面积较广、下垫面较复杂的影像,若用平均的气溶胶厚度和高程参数来对影像进行校正,将出现较大误差。提出了建立一种基于6S模型,以高程或气溶胶厚度为参数的大气校正模型与方法,并以广州Landsat ETM+为例,对校正前后的反射率直方图、NDVI灰度直方图以及各类地物的光谱特征进行分析。结果证明了该方法简单实用,校正精度高,可直接用于该地区相似气候条件下影像的大气校正,对类似的研究有借鉴意义。& 相似文献
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Tower-based spectral observation is an important connecting bridge between flux sites and satellite remote sensing data,and the effect of atmospheric absorption and scattering between horizontal surface and tower-based platform on the atmospheric absorption band such as O2-A is difficult to ignore.Firstly,the influence of atmospheric radiation transfer on the up-welling radiance and down-welling irradiance of the tower-based platform is analyzed,and the atmospheric correction method of based on upward and downward transmittance is established,that is,the influence of the upwelling radiance and down-welling irradiance is corrected by the direct transmittance and the total transmittance.Secondly,using the simulation data of MODTRAN model,the influence of AOD550 and radiative transfer path length on atmospheric transmittance is quantitatively analyzed,and the LUT of AOD550 is established based on the ratio of down-welling irradiance of near-infrared and red bands and solar zenith angle,as well as the upward and downward atmospheric transmittance LUT based on the AOD550 and the radiative transfer path length.Finally,using the canopy spectral data of different growth stages observed by the tower-based platform,the difference of the apparent reflectance between the inside and outside of the O2-A band absorption line before and after atmospheric correction was analyzed.The results show that the atmospheric correction method based on LUT of AOD550 and radiative transfer path length proposed in this paper can better correct the influence of upwelling radiance and down-welling on the O2-A absorption band of the tower-based platform,and provides important method support for applications such as SIF observation on the tower platform. 相似文献
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天宫一号(TG-1)搭载的高光谱成像仪获取了大量的高光谱数据,可用于国土资源、农林业和油气矿产等领域的研究。但由于遥感成像时会受到大气的干扰,因此需要首先进行大气校正,消除大气的影响,才能进行遥感定量分析与应用。利用准同步的中分辨率成像光谱仪MODIS(Moderate Resolution Imaging Spectroradiometer)大气参数产品,结合6S辐射传输模型对天宫一号高光谱成像仪数据进行大气校正,并利用地面测量光谱和同步MODIS反射率数据对结果进行了验证。结果表明:经过大气校正后,天宫一号高光谱成像仪数据和地面测量光谱一致性较好,所有样点的相关系数都大于0.97,最大均方根误差为0.088。和MODIS反射相比,各波段回归直线的斜率接近1,且R2都大于0.8。 相似文献
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水体光谱信息微弱,常用的基于辐射传输模型的大气校正方法在水体中校正精度较差。基于覆盖太湖水体的2016年4月29日的高分一号宽幅相机影像(GF-1/WFV)和同步的实测光谱数据,对6S辐射传输模型的输入参数进行敏感性分析,逐像元计算观测几何,使用分区气溶胶类型、分区暗像元和Spline插值确定的气溶胶光学厚度(Aerosol Optical Depth,AOD)进行6S逐像元大气校正。实验结果表明:气溶胶模式对6S大气校正结果的影响最大,与FLAASH方法相比,逐像元计算观测几何和气溶胶参数的校正方法对大气校正精度有改进作用,4个波段的平均相对误差分别降低了1.84%、7.78%、4.79%和17%。结合精确大气参数输入的6S逐像元大气校正方法可以改进水体表面遥感反射率的大气校正精度。 相似文献
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The spectral information of water is weak, and the commonly used radiation transfer model has poor accuracy in atmospheric correction of water body. Based on the Gaofen-1 WFV image (GF-1/WFV) and the synchronous in situ spectra covering Taihu Lake on 29th, April, 2016, the sensitivity analysis of the input parameters in 6S model was first performed, and then the image was corrected using 6S model using the observation geometry calculated pixel-by-pixel, the partitioned aerosol type and the Aerosol Optical Depth (AOD) determined by the partitioned dark pixel and Spline interpolation. The experimental results show that the aerosol type has the greatest influence on the 6S atmospheric correction results. Compared with the FLAASH method, the 6S method using the observation geometry and aerosol parameters calculated pixel-by-pixel significantly improved the atmospheric correction accuracy, with the ARE (Average Relative Error) of the four bands reduced by 1.84%,7.78%,4.79%,17%. The 6S atmospheric correction method pixel by pixel with the input of accurate atmospheric parameters can improve the correction accuracy of the remote sensing reflectance above water surface. 相似文献
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Shaoqi Gong Jiazhu Huang Yunmei Li Haijun Wang 《International journal of remote sensing》2013,34(8):2199-2210
In order to extract quantitative water‐leaving information from the Thematic Mapper (TM) image accurately in inland waters, atmospheric correction is a necessary step. Based on former researchers' results, the paper presents two atmospheric correction algorithms based on meteorological data (MD) and on Moderate Resolution Imaging Spectroradiometer (MODIS) Vicarious Calibration (MVC) for TM image in inland waters according to the theory of radiative transfer. Studying Taihu lake, China, in this paper we derived water remote sensing reflectance from a TM image of 26 July 2004 by these two atmospheric correction algorithms and we compare the results with that of dark object subtraction (DOS) and 6S code. The results show that the effect of atmospheric correction based on meteorological data and MODIS Vicarious Calibration is much better than that of DOS and 6S code. Although the MD is more accurate, MVC may be an ideal choice for TM images in inland water because TERRA MODIS images can be acquired easily than collecting meteorological data at the time of satellites passing over. 相似文献
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Luis Guanter Rudolf Richter Hermann Kaufmann 《International journal of remote sensing》2013,34(6):1407-1424
The quantification of atmospheric effects on the solar radiation measured by a spaceborne or airborne optical sensor is required for some key tasks in remote sensing, such as atmospheric correction, simulation of realistic scenarios or retrieval of atmospheric parameters. The MODTRAN4 code is an example of state‐of‐the‐art atmospheric radiative transfer code, as it provides very accurate calculations by means of a rigorous mathematical formulation and a very fine spectral resolution. However, the application of MODTRAN4 to remote sensing is not straightforward for the average user for a number of reasons: the provided output parameters do not exactly correspond to those necessary for the construction of the at‐sensor signal by combination with the surface reflectance, an advanced knowledge of radiative transfer theory and atmospheric physics is needed for the understanding of the input parameters and all their possible combinations, and the computation time may be too high for many practical applications. This work is intended to give explicit solutions to those problems. MODTRAN4 has been modified so that the proper atmospheric parameters are calculated and delivered as output. In addition, the most important execution options are investigated, and the compromise between accuracy and computation time is analysed. The performance of the proposed methodology is demonstrated by generating a look‐up table (LUT) enabling fast but accurate radiative transfer calculations for the atmospheric correction of data acquired by the Compact High Resolution Imaging Spectrometer (CHRIS) on board the Project for On‐Board Autonomy (PROBA). 相似文献