Abstract

In a previous publication [Di Girolamo et al., Appl. Opt. 45, 2474–2494 (2006)], certain information was printed inaccurately. These inaccuracies are corrected here.

© 2006 Optical Society of America

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References

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  1. P. Di Girolamo, A. Behrendt, and V. Wulfmeyer, "Spaceborne profiling of atmospheric temperature and particle extinction with pure rotational Raman lidar and of relative humidity in combination with differential absorption lidar: performance simulations," Appl. Opt. 45, 2474-2494 (2006).
    [CrossRef] [PubMed]

2006

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Equations (1)

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Δ α aer ( z ) α aer ( z ) = 100 2 Δ τ aer × [ ( P ref S + bk ref S ) ( P ref S + P ref AS ) 2 + ( P ref AS + bk ref AS ) ( P ref S + P ref AS ) 2 ] ,

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