Lidar: Range-Resolved Optical Remote Sensing of the Atmosphere

By C. Werner, J. Streicher. 2005

586 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/76d90be1dadc6a481253427715442c25e5f0ab0d

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Citations in the corpus

EARLINET correlative measurements for CALIPSO: First intercomparison results (2010, background): “Backscatter coefficients at three wavelengths plus extinction coefficients at two wavelengths (so ‐ called 3 + 2 measurements) are the minimum required input data for such inversion schemes [ Müller et al. , 2001; Veselovskii et al. , 2002; Böckmann et al. , 2005; Ansmann and Müller , 2005].”
Detection of Cloud-Base Height Using Jenoptik CHM15K and Vaisala CL31 Ceilometers (2010, background): “…of the lidar signal P(h) backscattered by an atmospheric layer of thickness Dh (range gate) centered at altitude h can be expressed in the form (Weitkamp 2005) P(h) 5 P L KO(h) A h2 Dhb(h)T2(h) 1 B, (1) where PL is the emitted optical power, K is the overall optical efficiency of the…”
Depolarization and lidar ratios at 355, 532, and 1064 nm and microphysical properties of aged tropospheric and stratospheric Canadian wildfire smoke (2018, methodology): “An overview of the retrieval methods is given in Ansmann and Müller (2005); Freudenthaler et al. (2009); and Freudenthaler (2016).”
An overview of the first decade of Polly NET : an emerging network of automated Raman-polarization lidars for continuous aerosol profiling (2016, background): “With multiwavelength-Raman-polarization lidars, aerosol layers can be characterized in terms of types, size distribution, and concentration (Ansmann and Müller, 2005; Müller et al., 2007; Ansmann et al., 2012).”
EARLINET: towards an advanced sustainable European aerosol lidar network (2014, background): “…Pappalardo et al. Title Page Abstract Introduction Conclusions References Tables Figures J I J I Back Close Full Screen / Esc Printer-friendly Version Interactive Discussion D iscussion P aper | D iscussion P aper | D iscussion P aper | D iscussion P aper | the path to that range (Weitkamp, 2005).”
An Analysis of the Performance of the UFAM Pulsed Doppler Lidar for Observing the Boundary Layer (2009, methodology): “FEBRUARY 2009 P E A R S O N E T A L . can be recorded followed by a vector analysis to yield the three components of the wind (u, y, and w) (Werner 2005).”