1. State Key Laboratory of Remote Sensing Science, Institute of Remote Sensing Applications, Chinese Academy of Sciences, Beijing 100101, China 2. Graduate University of Chinese Academy of Sciences, Beijing 100049, China 3. Demonstration Center of Spaceborne Remote Sensing, National Space Administration, Beijing 100101, China 4. State Environmental Protection Key Laboratory of Satellites Remote Sensing Applications, Beijing 100101, China
Abstract:The sea surface sunglint is caused by specular reflectance. Water is a kind of dark target with a very low reflectance, so sunglint becomes a big noise in the aerial or aerospace remote sensing images; sunglint is strongly polarized, and can be a natural standard light source for polarized sensor in-flight calibration; sunglint also can be utilized to retrieve gaseous constituents and aerosol properties. For both de-noising and being standard light source, the radiative physic parameters should be calculated accurately. First, A 3-D sea surface model was constituted according to the Cox & Munk model; Second, the polarized radiative model of sunglint was deduced based on the 3-D sea surface model and polarized Fresnel reflectance law; Third, the sensitivities of solar-viewing relative azimuth, zenith, wind speed and wind direction were analyzed utilizing the polarized radiative model. The polarization characteristics analysis of sunglint provides a theoretical basis for the quantitative remote sensing retrievals which uses sunglint.
Key words:Sunglint;Polarization;Remote sensing;Sea surface;DOLP (degree of linear polarization)
[1] Liou K N. An Introduction to Atmospheric Radiation-Second Edition. San Diego: Academic Press, 2002. 503. [2] Chen X F, Gu X F, Yin Q, et al. Proceedings of SPIE, 2009, 7498: 74980D. [3] Ottaviani M, Spurr R, Stamnes K, et al. Journal of Quantitative Spectroscopy & Radiative Transfer, 2008, 109: 2364. [4] Gordon H R. J. Geophys. Res., 1997, 102D: 17081. [5] Kleidman R G, Kaufman Y J, Gao B C, et al. Geophys. Res. Lett., 2000, 27: 2657. [6] Larsen N F, Stamnes K. Opt. Eng, 2006, 45: 016202-1. [7] Kaufman Y J, Martins J V, Remer L A, et al. Geophys. Res. Lett., 2002, 29(12): 34-1. [8] Toubbé B, Bailleul T, Deuzé J L, et al. IEEE Trans. Geosci. Remote Sensing, 1999, 37: 513. [9] CHENG Tian-hai, GU Xing-fa, CHEN Liang-fu, et al(程天海,顾行发,陈良富,等). Acta Phys. Sin.(物理学报), 2008, 57(8): 5323. [10] CHENG Tian-hai, GU Xing-fa, YU Tao, et al(程天海,顾行发,余 涛,等). Acta Phys. Sin.(物理学报), 2009, 58(10): 7368. [11] Deschamps P Y, Bréon F M, Leroy M, et al. IEEE Trans. Geosci. Remote Sensing, 1994, 32: 598. [12] WU Tai-xia, YAN Lei, XIANG Yun, et al (吴太夏,晏 磊,相 云,等). Spectroscopy and Spectral Analysis(光谱学与光谱分析), 2010, 30(2): 448. [13] Cox C, Munk W. Journal of Marine Research, 1954, 13(2): 198. [14] Cox C, Munk W. Journal of the Optical Society of America, 1954, 44(11): 838. [15] Cox C, Munk W. Journal of Marine Research, 1955, 14(1): 63. [16] Takashima T, Masuda K. Appl. Opt., 1985, 24(15): 2423. [17] Kawata Y, Yamazaki A. IEEE Trans. Geosci. Remote Sensing, 1998, 36: 51. [18] Theocaris P S. Matrix Theory of Photoelasticity. New York: Springer-Verlag, 1979. 18. [19] Leroy M, Deuzé L, Bréon F M, et al. J. Geophys. Res., 1997, 102: 17023. [20] Born M, Wolf E. Principles of Optics-Sixth Edition. New York: Pergamon Press, 1980. 40. [21] Li Z Q, Blarel L, Podvin T, et al. Appl. Opt., 2010, 49(8): 1249. [22] International Association for the Properties of Water and Steam http://www.iapws.org/Jun 13 2010. [23] TANG Jun-wu, TIAN Guo-liang, WANG Xiao-yong, et al(唐军武,田国良,汪小勇,等). Journal of Remote Sensing(遥感学报), 2004,8(1): 37. [24] Lenoble J, Herman M, Deuzé L, et al. Journal of Quantitative Spectroscopy & Radiative Transfer, 2007, 107: 479.