共查询到18条相似文献,搜索用时 109 毫秒
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1.315μm光解碘激光的大气透过率测量实验 总被引:4,自引:2,他引:2
利用1.315μm光解碘激光器在实际大气中作了大气透过率的测量,在中等能见度,相对湿度为64%和温度为21℃的条件下,平均透过率为0.78,同时用现有的数据库和计算程序作了计算比较,发现实验结果与计算值基本一致。 相似文献
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大气传输特性对目标与背景红外辐射特性的影响 总被引:12,自引:2,他引:10
本文对影响大气红外辐射透过率和大气自身的红外辐射因素及计算方法进行了讨论,利用大气传输特性分析软件-LOWTRAN7分析计算了大气红外辐射的透过率和大气自身的红外辐射,并讨论了大气辐射与吸收对目标与背景红外辐射特性的影响,对利用理论模型得到的目标与背景红外辐射图像进行了修正,获得了比较接近实际的红外模拟热图像。 相似文献
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被动微波遥感具有全天候工作的能力,但是在不同的大气状态下被动微波遥感受大气的影响不同。为了研究大气对高级微波扫描辐射计AMSR-E (advanced microwave scanning radiometer-earth observing system)入瞳亮温的影响,分别采用晴空和典型层云大气数据作为微波辐射传输模型的输入,进行大气微波辐射信号的模拟工作并分析大气的影响。结果表明晴空下大气水汽是引起大气辐射的主要因素,晴空条件下大气对典型被动微波传感器低频的(<18.7 GHz)透过率大于0.98,在整个辐射传输过程中可以忽略不计。36.5和89 GHz的大气透过率在晴空下分别为0.896和0.756,在用微波高频通道进行陆表参数反演时需进行大气水汽影响的校正; 云覆盖条件或者阴天情况下云中液态水是引起大气辐射的主要因素,典型层云覆盖下大气的透过率在10.7,18.7和36.5 GHz分别为0.942,0.828和0.605。与晴空相比,由层云中液态水引起的大气下行辐射的增量在36.5 GHz最大达到75.365 K。表明在云覆盖时大气影响的校正过程中云层的影响是校正重点。最后利用大气探空数据计算了内蒙古海拉尔地区2013年夏季7月份的大气透过率,结果显示C、X波段的大气透过率接近1,89 GHz受水汽影响较大,其地球表层大气透过率不超过0.7。在内蒙古海拉尔地区,夏季大气透过率具有较为稳定的值,但是随着局部水汽的变化具有0.1左右的波动。 相似文献
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大气模式与气溶胶模型对辐射传输计算的影响 总被引:1,自引:0,他引:1
大气模式与气溶胶模型选择是影响定量遥感应用的辐射传输计算的重要因素。人们一般凭感性认识去进行选择,有一定随意性,对其带来的影响程度关注甚少。以太阳辐射计测量为依据,对大气模式与气溶胶模型选择方法作了研究,并利用经辐射定标过的光谱辐射计地面测量对辐射传输计算精度进行了验证。在昆明进行的试验表明,在0.50~0.68μm范围内,选择中纬度冬季大气模式和大陆型气溶胶,经辐射传输计算后得到的光谱辐射亮度与光谱辐射计测量结果一致性很好,差别在3.3%以内;变换大气模式对辐射传输计算产生明显影响,差别达10%左右;选择不同的气溶胶模型对辐射传输计算影响也很大,差别达11%左右。基于辐射计测量的大气模式与气溶胶模型选择避免了主观选择的不可靠性,有益于减少辐射传输计算或卫星遥感大气订正的误差。 相似文献
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为了更准确地计算大气透过率,在Mie散射理论基础上,分析了雷达系统设计中需考虑的大气透过率的经验计算公式,指出了该经验公式的不足。考虑大气分析软件MODTRAN自身的优点,采用经验公式和软件计算相结合的方式计算大气透过率,给出了MODTRAN计算结果的修正表达式。在该理论指导下,进行了CO2激光大气传输实验。由于没有考虑大气湍流,理论计算和实验结果存在一定偏差,但不影响本文方法的实用性。实验测量显示,激光器出口处光斑能量抖动比为6.18%,而在50m和1km处能量抖动比分别为8.3%和50.2%,表明随着传输距离增加,能量抖动比增大。除掉激光器本身输出能量抖动外,在50m和1km处由大气传输造成的能量抖动比分别为2.12%和44.02%。实验结果提示,水平传输1km时能量抖动已相当剧烈,所以对更远距离的激光传输,自适应光学补偿显得尤为重要。 相似文献
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S. V. Yakovlev O. A. Romanovskii O. V. Kharchenko 《Bulletin of the Lebedev Physics Institute》2010,37(1):8-10
In this paper, we consider the applicability of the overtone CO laser to atmosphere gas analysis. The atmosphere transmittance
was calculated for lasing lines at the overtone frequencies of the CO laser. The results of the search for informative wavelengths
for sensing the minor gas components of the atmosphere N2O, NO2, H2CO, CH4, C2H2, HCl, HBr, and HCN are presented. 相似文献
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F.W. Taylor 《Journal of Quantitative Spectroscopy & Radiative Transfer》1973,13(11):1181-1217
Data are presented on the positions, intensities, half widths and ground state energies of approximately 1700 of the strongest spectral limes in the ν2 band of ammonia and its first overtone. The values are used to compute the transmission function for dilute mixtures of ammonia in hydrogen, approximating the Jovian environment, and these are compored to laboratory measured transmissions for the same conditions. The application of the data to theoretical studies of radiative transfer in the atmosphere of Jupiter and the interpretation of observations in the 8–20 μ range is discussed. 相似文献
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C.F. Wisniewski K.B. Hewett G.C. Manke II P.G. Crowell C.R. Truman G.D. Hager 《Applied Physics A: Materials Science & Processing》2003,77(2):337-342
The overtone gain medium of a small-scale HF overtone laser was probed using a sub-Doppler tunable diode laser. Two-dimensional
spatially resolved small signal gain and temperature maps were generated for several ro-vibrational transitions in the HF
(v=2→v=0) overtone band. Our results compare well with previous measurements of the overtone gain in a similar HF laser device.
Received: 7 October 2002 / Accepted: 20 January 2003 / Published online: 28 May 2003
RID="*"
ID="*"Corresponding author. Fax: +1-505/846-4807, E-mail: kevin.hewett@kirtland.af.mil 相似文献
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提出了一种基于单帧多波段图像测量非气体吸收波段和弱气体吸收波段大气透过率的方法,可应用于相关光电工程中评估和修正大气衰减影响.首先,利用经过绝对辐射定标的图像采集设备获得辐射图像;其次,基于大气中图像退化光学模型与暗通道先验统计理论得到辐射图像暗通道对应的宽波段平均大气透过率;最后,结合特定波段消光系数和宽波段平均消光系数间的关系得到特定波段的大气透过率.实验对比分析表明:本文方法与能见度仪、激光雷达测量结果相关性较高,其中与能见度仪相比,相关系数在0.89和0.95之间,与激光雷达相比,相关系数在0.95和0.97之间;在1km近距离条件下与能见度仪、激光雷达测量结果平均相对偏差最高分别为9%和6%,在远距离条件下,与能见度仪测量结果相比,4km和6km平均相对偏差最高分别为15%和30%,与激光雷达测量结果相比,4km和6km平均相对偏差最高分别为9%和18%. 相似文献
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Eugene A. Ustinov 《Journal of Quantitative Spectroscopy & Radiative Transfer》2007,103(1):217-230
In two recent papers, referred to as Paper 1 and Paper 2 in the main text, we have pursued an idea that atmospheric weighting functions for any geophysical parameters essentially consist of two kinds of entities: weighting functions for the atmospheric radiative parameters, which directly enter the radiative transfer equation, and partial derivatives of the atmospheric radiative parameters with respect to atmospheric geophysical parameters. Corresponding analysis was performed for non-scattering and scattering planetary atmospheres for nadir-viewing geometry and thermal spectral region. In the present paper we conduct a study of the second group of above entities, the partial derivatives of atmospheric radiative parameters with respect to atmospheric geophysical parameters. Along the way, we analyze the role of radiative parameters of individual atmospheric constituents, which serve as intermediaries between the total radiative parameters of the atmosphere and its geophysical parameters. The obtained expressions, combined with radiative weighting functions, are used in the end-to-end expressions for the weighting functions obtained for various specific geophysical parameters. 相似文献
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海洋水色水温扫描仪(COCTS)是中国海洋水色系列卫星上的主遥感器,主要用于探测我国及全球部分海域的海洋水色和水温环境信息.大气漫射透射比计算是COCTS大气校正的必需过程,直接影响COCTS大气校正和水色信息反演的精度.提出了基于加倍法解大气-海洋耦合矢量辐射传输方程的大气漫射透射比精确计算方法,通过与SeaWiFS精确大气漫射透射比查找表计算结果的比较,结果表明计算相对误差小于1.5%,而当观测天顶角小于60°时,计算相对误差小于0.5%,可以用来生成COCTS的精确大气漫射透射比查找表.在此基础上,生成了专门针对COCTS的精确大气漫射透射比查找表. 相似文献
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The laser detection technology in uncertain and dynamic environments is of utmost importance in many fields. A model of transient radiative transfer of bidirectional path laser based on Monte Carlo method is developed to investigate the optimum wavelength of active detector at complex atmospheric conditions. The radiative parameters of atmosphere are calculated by HITRAN database and Mie theory at several typical atmospheric conditions including the standard atmosphere, urban aerosol, and radiation fog. Transmission characteristics for five spectral bands at the above atmospheric conditions are calculated by this model. The optimal transmission ability occurred in bands 0.2–0.5, 1.4–1.6, and 0.75–1.25 μm on the condition of standard atmosphere, urban aerosol, and radiation fog, respectively. All results provide effective reference and basic support for choosing the optimal spectral band for active detection. 相似文献