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In the process of wind retrieval for Rayleigh Doppler lidar, besides atmospheric temperature and pressure, the accuracy of the wind retrieval result is also affected by Mie signal. When the Mie scattering sigal is large, especially in the cases such as high altitude clouds or volcanic ash and so on, the wind retrieval result will largely deviate from the ture value if the aerosol signal is ignored due to temperature uncertainty and Mie signal contamination. A nonlinear iterative algorithm is proposed, which can retrieve both wind and atmospheric temperature by using the mesured signal with outgoing laser pointing to the zenith. The initial operating point of laser is optimized. Simulation results show that the proposed algorithm can retrieve scattering ratio effectively, and by combination with the nonlinear iterative algorithm of wind retrieval, this algorithm can eliminate the effect of aerosol backscattering signal and then improve the atmopheric wind speed and the temperature retrieval accuracy effectively.
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Keywords:
- lidar /
- Rayleigh scattering /
- Doppler /
- Fabry-Perot etalon
[1] Gentry B M, Chen H L, Li S X 2000 Opt. Lett. 25 1231
[2] Flesia C, Korb C L, Hirt C 2000 Opt. Lett. 25 1466
[3] Korb C L, Flesia C 1999 Appl. Opt. 38 432
[4] Dabas A, Denneulin M L, Flamant P, Loth C, Garnier A, Dofli-Bouteyre A 2007 Tellus 60 206
[5] ESA 2008 ADM-Aeolus Science Report ESA SP-1311
[6] Souprayen C, Garnier A, Hertzog A, Hauchecorne A, Porteneuve J 1999 Appl. Opt. 38 2410
[7] Souprayen C, Garnier A, Hertzog A, Hauchecorne A, Porteneuve J 1999 Appl. Opt. 38 2422
[8] Shen F H, Cha H K, Dong J H, Kim D H, Sun D S, Kwon S O 2009 Chin. Opt. Lett. 7 593
[9] Tang L Shu Z F, Dong J H, Wang G C Wang Y T, Xu W J, Hu D D, Chen T D Dou X K, Sun D S, Cha H K 2010 Chin. Opt. Lett. 8 726
[10] Shen F H, Shu Z F, Sun D S,Wang Z C, Xue X H, Chen T D, Dou X K 2011 Acta Phys. Sin. 60 060704 (in Chinese)[沈法华,舒志峰,孙东松,王忠纯,薛向辉,陈廷娣,窦贤康 2011 物理学报 60 060704]
[11] McGill M J, Skinner W R, Irgang T D 1997 Appl. Opt. 36 1253
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[1] Gentry B M, Chen H L, Li S X 2000 Opt. Lett. 25 1231
[2] Flesia C, Korb C L, Hirt C 2000 Opt. Lett. 25 1466
[3] Korb C L, Flesia C 1999 Appl. Opt. 38 432
[4] Dabas A, Denneulin M L, Flamant P, Loth C, Garnier A, Dofli-Bouteyre A 2007 Tellus 60 206
[5] ESA 2008 ADM-Aeolus Science Report ESA SP-1311
[6] Souprayen C, Garnier A, Hertzog A, Hauchecorne A, Porteneuve J 1999 Appl. Opt. 38 2410
[7] Souprayen C, Garnier A, Hertzog A, Hauchecorne A, Porteneuve J 1999 Appl. Opt. 38 2422
[8] Shen F H, Cha H K, Dong J H, Kim D H, Sun D S, Kwon S O 2009 Chin. Opt. Lett. 7 593
[9] Tang L Shu Z F, Dong J H, Wang G C Wang Y T, Xu W J, Hu D D, Chen T D Dou X K, Sun D S, Cha H K 2010 Chin. Opt. Lett. 8 726
[10] Shen F H, Shu Z F, Sun D S,Wang Z C, Xue X H, Chen T D, Dou X K 2011 Acta Phys. Sin. 60 060704 (in Chinese)[沈法华,舒志峰,孙东松,王忠纯,薛向辉,陈廷娣,窦贤康 2011 物理学报 60 060704]
[11] McGill M J, Skinner W R, Irgang T D 1997 Appl. Opt. 36 1253
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