Alejandro Rodríguez-GómezFrancesc RocadenboschMichaël SicardDiego LangeRubén BarragánÒscar BatetAdolfo ComerónMiguel Ángel López MárquezConstantino Muñoz-PorcarJordi Tiana‐Alsina2026-03-222026-03-22201510.1088/1755-1315/28/1/012013https://doi.org/10.1088/1755-1315/28/1/012013https://andeanlibrary.org/handle/123456789/54704Citaciones: 3Elastic lidars provide range-resolved information about the aerosol content in the atmosphere. Nevertheless, a number of pre-processing techniques need to be used before performing the inversion of the detected signal: range-correction, time-averaging, photoncounting channel dead-time correction, overlap correction, Rayleigh-fitting and gluing of both channels.enAerosolLidarRayleigh scatteringInversion (geology)Remote sensingWavelengthAtmospheric opticsSignal processingSIGNAL (programming language)Channel (broadcasting)article