2012
DOI: 10.1007/s00340-012-5040-7
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Remote sensing of trace gases with optical correlation spectroscopy and lidar: theoretical and numerical approach

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Cited by 11 publications
(8 citation statements)
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“…(1), an integral is performed over an effective wavelength spectral range Dk, defined from the effective width of the amplitude modulation function; therefore, the OCS-lidar methodology does not require a spectrally resolved detector. From the two OCS-lidar signals P C and P NC , a calculus detailed in B. Thomas et al [20] is then performed to retrieve absolute range-resolved atmospheric gas concentrations, with statistical and systematical error assessment. It is important to note that this OCS-lidar methodology does not require a permanent gas calibration as in regular optical correlation spectroscopy [32].…”
Section: The Ocs-lidar Principlementioning
confidence: 99%
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“…(1), an integral is performed over an effective wavelength spectral range Dk, defined from the effective width of the amplitude modulation function; therefore, the OCS-lidar methodology does not require a spectrally resolved detector. From the two OCS-lidar signals P C and P NC , a calculus detailed in B. Thomas et al [20] is then performed to retrieve absolute range-resolved atmospheric gas concentrations, with statistical and systematical error assessment. It is important to note that this OCS-lidar methodology does not require a permanent gas calibration as in regular optical correlation spectroscopy [32].…”
Section: The Ocs-lidar Principlementioning
confidence: 99%
“…3 experiment, we here perform a numerical simulation using the OCS-lidar methodology for water vapor concentration retrievals to optimize the precision on the retrieved concentration. We use the numerical model developed in B. Thomas et al [20] to generate OCS-lidar signals. This numerical model has four main inputs: the water vapor absorption crosssection spectrum plotted in Fig.…”
Section: Simulation Of Ocs-lidar Measurementmentioning
confidence: 99%
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