• Infrared and Laser Engineering
  • Vol. 36, Issue 3, 369 (2007)
1,*, 2, 3, 1, and 1
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  • 1[in Chinese]
  • 2[in Chinese]
  • 3[in Chinese]
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    [in Chinese], [in Chinese], [in Chinese], [in Chinese], [in Chinese]. Two-dimensional distribution of aerosol measured by lidar[J]. Infrared and Laser Engineering, 2007, 36(3): 369 Copy Citation Text show less
    References

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    [4] FERNALD F G.Analysis of atmospheric lidar observation:some comments[J].Appl Opt,1984,23(5):652-653.

    [5] TAKAMURA T,SASANO Y.Ratio of aerosol backscatter to extinction coefficients as determined from angular scattering measurements for use in atmospheric lidar applications[J].Optical and Quantum Electronics.1987,19:293-302.

    [6] LEFRERE J.Lidar survey of the post Mt.St.Helens stratospheric aerosol at Haule Province Observatory[J].Appl Opt,1981,20(7):1116-1117.

    [7] TOMINE K HIRAYAMA C,MICHIMOTO K et al.Experimental determination of the crossover function in the laser radar equation for days with a light mist[J].Appl Opt,1989,28(12):2194-2195.

    [8] DHO S W,PARK Y J,KONG H J.Experimental determination of ageometric form factor in the lidar equation for an inhomogeneous atmosphere[J].Appl 0pt,1997,36(24):6009-6010.

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    [in Chinese], [in Chinese], [in Chinese], [in Chinese], [in Chinese]. Two-dimensional distribution of aerosol measured by lidar[J]. Infrared and Laser Engineering, 2007, 36(3): 369
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