Sensitivity analysis of differential absorption lidar measurements in the mid-infrared region

2000 ◽  
Vol 39 (36) ◽  
pp. 6847 ◽  
Author(s):  
Paolo Francesco Ambrico ◽  
Aldo Amodeo ◽  
Paolo Di Girolamo ◽  
Nicola Spinelli
2004 ◽  
Vol 43 (26) ◽  
pp. 5092 ◽  
Author(s):  
Grady J. Koch ◽  
Bruce W. Barnes ◽  
Mulugeta Petros ◽  
Jeffrey Y. Beyon ◽  
Farzin Amzajerdian ◽  
...  

1998 ◽  
Vol 66 (1) ◽  
pp. 105-113 ◽  
Author(s):  
M.J.T. Milton ◽  
G. Ancellet ◽  
A. Apituley ◽  
J. B�senberg ◽  
W. Carnuth ◽  
...  

2021 ◽  
Vol 14 (10) ◽  
pp. 6675-6693
Author(s):  
Jonas Hamperl ◽  
Clément Capitaine ◽  
Jean-Baptiste Dherbecourt ◽  
Myriam Raybaut ◽  
Patrick Chazette ◽  
...  

Abstract. Laser active remote sensing of tropospheric water vapor is a promising technology to complement passive observational means in order to enhance our understanding of processes governing the global hydrological cycle. In such a context, we investigate the potential of monitoring both water vapor H216O and its isotopologue HD16O using a differential absorption lidar (DIAL) allowing for ground-based remote measurements at high spatio-temporal resolution (150 m and 10 min) in the lower troposphere. This paper presents a sensitivity analysis and an error budget for a DIAL system under development which will operate in the 2 µm spectral region. Using a performance simulator, the sensitivity of the DIAL-retrieved mixing ratios to instrument-specific and environmental parameters is investigated. This numerical study uses different atmospheric conditions ranging from tropical to polar latitudes with realistic aerosol loads. Our simulations show that the measurement of the main isotopologue H216O is possible over the first 1.5 km of atmosphere with a relative precision in the water vapor mixing ratio of <1 % in a mid-latitude or tropical environment. For the measurement of HD16O mixing ratios under the same conditions, relative precision is found to be slightly lower but still sufficient for the retrieval of range-resolved isotopic ratios with precisions in δD of a few per mil. We also show that expected precisions vary by an order of magnitude between tropical and polar conditions, the latter giving rise to poorer sensitivity due to low water vapor content and low aerosol load. Such values have been obtained for a commercial InGaAs PIN photodiode, as well as for temporal and line-of-sight resolutions of 10 min and 150 m, respectively. Additionally, using vertical isotopologue profiles derived from a previous field campaign, precision estimates for the HD16O isotopic abundance are provided for that specific case.


Sensors ◽  
2020 ◽  
Vol 20 (8) ◽  
pp. 2211
Author(s):  
Yu Gong ◽  
Lingbing Bu ◽  
Bin Yang ◽  
Farhan Mustafa

Developments in mid-infrared Differential Absorption Lidar (DIAL), for gas remote sensing, have received a significant amount of research in recent years. In this paper, a high repetition rate tunable mid-infrared DIAL, mounted on a mobile platform, has been built for long range remote detection of gas plumes. The lidar uses a solid-state tunable optical parametric oscillator laser, which can emit laser pulse with repetition rate of 500 Hz and between the band from 2.5 μm to 4 μm. A monitoring channel has been used to record the laser energy in real-time and correct signals. Convolution correction technology has also been incorporated to choose the laser wavelengths. Taking NO2 and SO2 as examples, lidar system calibration experiment and open field observation experiment have been carried out. The observation results show that the minimum detection sensitivity of NO2 and SO2 can reach 0.07 mg/m3, and 0.31 mg/m3, respectively. The effective temporal resolution can reach second level for the high repetition rate of the laser, which demonstrates that the system can be used for the real-time remote sensing of atmospheric pollution gas.


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