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Wavelet correlation transform method and gradient method to determine aerosol layering from lidar returns: Some comments

Autor
Comeron, A.; Sicard, M.; Rocadenbosch, F.
Tipus d'activitat
Article en revista
Revista
Journal of atmospheric and oceanic technology
Data de publicació
2013-06
Volum
30
Número
6
Pàgina inicial
1189
Pàgina final
1193
DOI
https://doi.org/10.1175/JTECH-D-12-00233.1 Obrir en finestra nova
Repositori
http://hdl.handle.net/2117/87070 Obrir en finestra nova
URL
http://journals.ametsoc.org/doi/abs/10.1175/JTECH-D-12-00233.1 Obrir en finestra nova
Resum
Identification of aerosol layers on lidar measurements is of interest to determine ranges where aerosol properties are likely to be homogeneous and to infer transport phenomena and atmosphere dynamics. For instance, the range-corrected backscattered signal from aerosol measured with lidars has long been used as a proxy to determine the depth of the planetary boundary layer. The method relies on the assumption that in a well-mixed atmosphere, a rather homogenous aerosol distribution will exist wi...
Citació
Comeron, A., Sicard, M., Rocadenbosch, F. Wavelet correlation transform method and gradient method to determine aerosol layering from lidar returns: Some comments. "Journal of atmospheric and oceanic technology", Juny 2013, vol. 30, núm. 6, p. 1189-1193.
Paraules clau
Aerosol Distribution, Atmosphere Dynamics, Backscattered Signal, Boundary Layer Heights, Correlation Function, Lofted Aerosol Layers, Planetary Boundary Layers, Transport Phenomena
Grup de recerca
RSLAB - Grup de Recerca en Teledetecció

Participants