浏览全部资源
扫码关注微信
纸质出版日期： 2019-3 ，
录用日期： 2017-9-19
扫 描 看 全 文
陈震霆, 孙晓兵, 汪俊锋, 李树, 黄红莲, 陈卫, 乔延利. 2019. 近红外偏振辐射卫星数据的海洋耀光动态检测. 遥感学报, 23(2): 215–229
Chen Z T, Sun X B, Wang J F, Li S, Huang H L, Chen W and Qiao Y L. 2019. Dynamic detection of ocean glint from near-infrared polarized radiation satellite data. Journal of Remote Sensing, 23(2): 215–229
太阳光入射海表特定区域形成海洋耀光，呈强反射和偏振特性。在卫星海洋遥感中，海洋耀光对遥感成像质量有较大影响，尤其对海洋上空云、气溶胶及海色等研究干扰较大，因此剔除海洋耀光是卫星遥感数据处理过程中首先要解决的重要问题。以PARASOL卫星的POLDER3载荷数据为研究对象，获取载荷成像时刻太阳及观测几何、海表风速风向及气溶胶光学厚度等参数，采用海气辐射传输相关理论，结合耀光角和多角度NIR偏振辐射信息(865 nm)，构建基于近红外偏振辐射特性规则的OGDD模型，获取耀光角临界值实现耀光动态检测。以印度洋某海区为研究对象，获取实测耀光区NIR通道的大气层顶反射率和偏振反射率，利用OGDD模型将耀光角判别临界值调整为34°。相比MODIS经验临界值(40°)，标记耀光像元相对减少了30%。结果表明，该方法不仅能通过动态调整临界值准确识别海洋耀光，为云检测及云物理特性反演提供可靠的源数据，还能为高分五号卫星多角度偏振载荷在轨定标及气溶胶反演提供支持。
Sunlight incoming sea surface forms ocean glint (OG) in a special area and shows strong reflection and polarization characteristics. OG significantly influences the imaging quality of ocean remote sensing
especially because the interference is large for clouds and aerosols above the ocean surface. Therefore
eliminating OG is the key problem to be solved in the process of remote sensing data. At present
most OG detections of sensors are utilized by a rough sea surface polarization model combined with an empirical threshold. Orbit height and resolution is different from various sensors available. Thus
the result is quite inaccurate using the same threshold to discriminate glint pixels
thereby resulting in several pixels being utilized ineffectively. The Chinese GF-5 satellite has been scheduled for launch in 2017. It carries a Directional Polarimetric Camera (DPC) sensor for the atmospheric polarization research at a global scale. Similarly
the OG detection is essential to DPC data processing. The traditional method cannot achieve the dynamic detection of OG for different satellite data. Thus
the problem of accurately obtaining a threshold angle has become the key difficulty of OG dynamic detecting research. OG dynamic detecting (OGDD) method was proposed on the basis of near-infrared (NIR) polarized data
which were not easily affected by atmospheric disturbance under a clear sky. From these data
several parameters
such as the geometry conditions of solar and observation and sea surface wind speed and direction
could be obtained. According to ocean–atmosphere coupled radiative transfer theory
the OGDD model
combined with the OG and multi-directional NIR-polarized radiation information (865 nm)
was developed on the basis of the regular performance of the NIR-polarized radiation characteristic. The OGDD was realized by obtaining the dynamic threshold of a glint angle. A calibration layer was selected by using the polarized characteristic tendency of an OG center from detecting layers
and after cloudy pixels have been removed
a slope dynamic analysis was conducted on the basis of an OG-polarized radiative regular variety on top of the atmosphere. Finally
the ocean pixels were marked as glint pixels using the dynamic threshold of the glint angle. This study used PARASOL/POLDER3 satellite data as the research object for the DPC simulation and selected the Indian Ocean as the study area. The NIR channel utilized the OGDD model to acquire apparent and polarization reflectivity (865 nm) of the sea surface. The glint threshold was adjusted dynamically to 34° using the OGDD model. In comparison with MODIS 40°
the glint angle was reduced by approximately 15%
and the pixel-marked glint was relatively decreased by 30%. Similarly
in comparison with POLDER3 30°
the glint angle was relatively improved by nearly 13%
and the pixel-marked glint was increased by 30%. The model can effectively distinguish the glint and non-glint pixels through a dynamically adjusted threshold and significantly improve the utilization rate of the pixels by reducing the interference of aerosol retrieval at the clear sky area. Furthermore
this model can generate reliable data for cloud detection and microphysical characteristic retrieval and provide support to developing the in-flight calibration and aerosol inversion of the GF-5 satellite multi-angle polarization sensor.
PARASOL海气辐射海洋耀光辐射信息偏振反射率动态检测高分五号偏振遥感
PARASOLocean-atmosphere coupled radiationocean glintradiation informationpolarized reflectanceOcean Glint Dynamic DetectingGF-5polarization remote sensing
Born M and Wolf E. 1975. Principles of Optics. 7th ed. New York: Pergamon Press: 50–65
Bréon F M. 1993. An analytical model for the cloud-free atmosphere/ocean system reflectance. Remote Sensing of Environment, 43(2): 179–192
Bréon F M and Henriot N. 2006. Spaceborne observations of ocean glint reflectance and modeling of wave slope distributions. Journal of Geophysical Research: Oceans, 111(C6): C06005
Bréon F M, Tanré D, Lecomte P and Herman M. 1995. Polarized reflectance of bare soils and vegetation: measurements and models. IEEE Transactions on Geoscience and Remote Sensing, 33(2): 487–499
Buriez J C, Vanbauce C, Parol F, Goloub P, Herman M, Bonnel B, Fouquart Y, Couvert P and Seze G. 1997. Cloud detection and derivation of cloud properties from POLDER. International Journal of Remote Sensing, 18(13): 2785–2813
陈兴峰, 顾行发, 程天海, 李正强, 余涛, 谢东海. 2011. 真实海洋表面的太阳耀光偏振辐射特性仿真与分析. 光谱学与光谱分析, 31(6): 1648–1653
Chen X F, Gu X F, Cheng T H, Li Z Q, Yu T and Xie D H. 2011. Simulation and analysis of polarization characteristics for real sea surface sunglint. Spectroscopy and Spectral Analysis, 31(6): 1648–1653 (
Cox C and Munk W. 1954a. Measurements of the roughness of the sea surface from photographs of the sun’s glitter. Journal of the Optical Society of America, 44(11): 838–850
Cox C and Munk W. 1956. Slopes of the sea surface deduced from photographs of sun glitter. Bulletin of the Scripps Institution of Oceanography, 6(9): 401–488
Cox C and Munk W. 1955. Some problems in optical oceanography. Journal of Marine Research, 14: 63–78
Cox C and Munk W H. 1954b. Statistics of the sea surface derived from sun glitter. Journal of Marine Research, 13: 198–227
Deschamps P Y, Bréon F M, Leroy M, Podaire A, Bricaud A, Buriez J C and Seze G. 1994. The POLDER mission: instrument characteristics and scientific objectives. IEEE Transactions on Geoscience and Remote Sensing, 32(3): 598–615
Deuzé J L, Bréon F M and Devaux C, Goloub P, Herman M, Lafrance B, Maignan F, Marchand A, Nadal F, Perry G and Tanré D. 2001. Remote sensing of aerosols over land surfaces from POLDER-ADEOS-1 polarized measurements. Journal of Geophysical Research, 106(D5): 4913–4926
Goloub P, Chepfer H, Herman M, Brogniez G and Parol F. 1997. Use of polarization for cloud study//Proceedings of Polarization: Measurement, Analysis, and Remote Sensing. San Diego, CA, United States: SPIE, 3121: 330–341 [DOI: 10.1117/12.283865]
Goloub P, Herman M and Parol F. 1995. Polarization of clouds//Proceedings of Atmospheric Sensing and Modeling II. Paris, France: SPIE, 2582: 21–31 [DOI: 10.1117/12.228551]
Gordon H R and Wang M. 1994. Influence of oceanic whitecaps on atmospheric correction of ocean-color sensors. Applied Optics, 33(33): 7754–7763
顾行发, 程天海, 李正强, 乔延利. 2015. 大气气溶胶偏振遥感. 北京: 高等教育出版社: 1–22
Gu X F, Cheng T H, Li Z Q, Qiao Y L. 2015. Atmospheric aerosol polarized remote sensing. Beijing: Higher Education Press: 1–22
Hagolle O, Nicolas J M, Fougnie B, Cabot F and Henry P. 2004. Absolute calibration of VEGETATION derived from an interband method based on the sun glint over ocean. IEEE Transactions on Geoscience and Remote Sensing, 42(7): 1472–1481
Harmel T and Chami M. 2013. Estimation of the sunglint radiance field from optical satellite imagery over open ocean: multidirectional approach and polarization aspects. Journal of Geophysical Research: Oceans, 118(1): 76–90
Koepke P. 1984. Effective reflectance of oceanic whitecaps. Applied Optics, 23(11): 1816–1824
Kotchenova S Y and Vermote E F. 2007. Validation of a vector version of the 6S radiative transfer code for atmospheric correction of satellite data. Part II. Homogeneous Lambertian and anisotropic surfaces. Applied Optics, 46(20): 4455–4464
Li Z Q, Goloub P, Devaux C, Gu X F, Deuzé J L, Qiao Y L and Zhao F S. 2006. Retrieval of aerosol optical and physical properties from ground-based spectral, multi-angular, and polarized sun-photometer measurements. Remote Sensing of Environment, 101(4): 519–533
Liou K N. 2002. An Introduction to Atmospheric Radiation. 2nd ed. USA: Elsevier: 200–255
毛志华, 郭德方, 潘德炉. 1996. 航空水色遥感中太阳耀光信息提取及消除方法的研究. 遥感技术与应用, 11(4): 15–20
Mao Z H, Guo D F and Pan D L. 1996. A study of sun glitter obtaining and removing in air-borne ocean color remote sensing. Remote Sensing Technology and Application, 11(4): 15–20 (
潘德炉, 李淑菁, 毛天明. 1997. 卫星海洋水色遥感的辐射模式研究. 海洋与湖沼, 28(6): 652–658
Pan D L, Li S J and Mao T M. 1997. Study on radiance models for ocean colour remote sensing. Oceanologia et Limnologia Sinica, 28(6): 652–658 (
伽丽丽, 马䶮, 陈兴峰, 李莉, 李正强, 张洋. 2016. 卫星近红外偏振通道反演气溶胶光学厚度的气溶胶模型影响. 红外与毫米波学报, 35(5): 569–577
Qie L L, Ma Y, Chen X F, Li L, Li Z Q and Zhang Y. 2016. Aerosol model assumption: the retrievals of aerosol optical depth from satellite near-infrared polarimetric measurements. Journal of Infrared and Millimeter Waves, 35(5): 569–577 (
Remer L A, Kaufman Y J, Tanré D, Mattoo S, Chu D A, Martins J V, Li R R, Ichoku C, Levy R C, Kleidman R G, Eck T F, Vermote E and Holben B N. 2005. The MODIS aerosol algorithm, products, and validation. Journal of the Atmospheric Sciences, 62(4): 947–973
Riédi J, Marchant B, Platnick S, Baum B A, Thieuleux F, Oudard C, Parol F, Nicolas J M and Dubuisson P. 2010. Cloud thermodynamic phase inferred from merged POLDER and MODIS data. Atmospheric Chemistry and Physics, 10(23): 11851–11865
Toubbe B, Bailleul T, Deuze J L Goloub P, Hagolle O and Herman M. 1999. In-flight calibration of the POLDER polarized channels using the sun’s glitter. IEEE Transactions on Geoscience and Remote Sensing, 37(1): 513–524
相关作者
相关机构
京公网安备11010802024621