Articles | Volume 9, issue 3
https://doi.org/10.5194/amt-9-1399-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/amt-9-1399-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Observations of water vapor mixing ratio profile and flux in the Tibetan Plateau based on the lidar technique
Songhua Wu
CORRESPONDING AUTHOR
Ocean Remote Sensing Institute, Ocean University of
China, Qingdao, China
Guangyao Dai
Ocean Remote Sensing Institute, Ocean University of
China, Qingdao, China
Xiaoquan Song
Ocean Remote Sensing Institute, Ocean University of
China, Qingdao, China
Bingyi Liu
Ocean Remote Sensing Institute, Ocean University of
China, Qingdao, China
Liping Liu
Laboratory of Severe Weather, Chinese Academy of
Meteorological Science, Beijing, China
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Cited
14 citations as recorded by crossref.
- Optical and Geometrical Properties of Cirrus Clouds over the Tibetan Plateau Measured by LiDAR and Radiosonde Sounding during the Summertime in 2014 G. Dai et al. 10.3390/rs11030302
- Validation of Water Vapor Vertical Distributions Retrieved from MAX-DOAS over Beijing, China H. Lin et al. 10.3390/rs12193193
- Classification of Cloud Phase Using Combined Ground-Based Polarization Lidar and Millimeter Cloud Radar Observations Over the Tibetan Plateau Y. Bian et al. 10.1109/TGRS.2023.3313798
- Statistics of optical and geometrical properties of cirrus cloud over tibetan plateau measured by lidar and radiosonde G. Dai et al. 10.1051/epjconf/201817605040
- Ground-based vertical profile observations of atmospheric composition on the Tibetan Plateau (2017–2019) C. Xing et al. 10.5194/essd-13-4897-2021
- Compact fiber-optic spectroscopic design and its validation in atmospheric water vapor Raman lidar Y. Wang et al. 10.1364/JOSAB.384944
- Vertical Structure of Air Pollutant Transport Flux as Determined by Ground-Based Remote Sensing Observations in Fen-Wei Plain, China X. Ji et al. 10.3390/rs13183664
- Distinct impacts of humidity profiles on physical properties and secondary formation of aerosols in Shanghai T. Liu et al. 10.1016/j.atmosenv.2021.118756
- Retrieval and Calculation of Vertical Aerosol Mass Fluxes by a Coherent Doppler Lidar and a Sun Photometer X. Wang et al. 10.3390/rs13163259
- The investigation of retrieval method for aerosol and water vapor profiles based on MAX-DOAS technology C. Zhou et al. 10.1016/j.apr.2024.102183
- Shipborne Wind Measurement and Motion-induced Error Correction of a Coherent Doppler Lidar over the Yellow Sea in 2014 X. Zhai et al. 10.5194/amt-11-1313-2018
- The Evolution of Springtime Water Vapor Over Beijing Observed by a High Dynamic Raman Lidar System: Case Studies T. Su et al. 10.1109/JSTARS.2017.2653811
- Investigation of the Spatial and Temporal Variation of Temperature and Water Vapor in Lower Troposphere Using the Combined Backward Raman Scattering LiDAR and Lateral Scanning Raman Scattering LiDAR F. Yang et al. 10.1109/TGRS.2024.3467340
- Raman lidar water vapor profiling over Warsaw, Poland I. Stachlewska et al. 10.1016/j.atmosres.2017.05.004
14 citations as recorded by crossref.
- Optical and Geometrical Properties of Cirrus Clouds over the Tibetan Plateau Measured by LiDAR and Radiosonde Sounding during the Summertime in 2014 G. Dai et al. 10.3390/rs11030302
- Validation of Water Vapor Vertical Distributions Retrieved from MAX-DOAS over Beijing, China H. Lin et al. 10.3390/rs12193193
- Classification of Cloud Phase Using Combined Ground-Based Polarization Lidar and Millimeter Cloud Radar Observations Over the Tibetan Plateau Y. Bian et al. 10.1109/TGRS.2023.3313798
- Statistics of optical and geometrical properties of cirrus cloud over tibetan plateau measured by lidar and radiosonde G. Dai et al. 10.1051/epjconf/201817605040
- Ground-based vertical profile observations of atmospheric composition on the Tibetan Plateau (2017–2019) C. Xing et al. 10.5194/essd-13-4897-2021
- Compact fiber-optic spectroscopic design and its validation in atmospheric water vapor Raman lidar Y. Wang et al. 10.1364/JOSAB.384944
- Vertical Structure of Air Pollutant Transport Flux as Determined by Ground-Based Remote Sensing Observations in Fen-Wei Plain, China X. Ji et al. 10.3390/rs13183664
- Distinct impacts of humidity profiles on physical properties and secondary formation of aerosols in Shanghai T. Liu et al. 10.1016/j.atmosenv.2021.118756
- Retrieval and Calculation of Vertical Aerosol Mass Fluxes by a Coherent Doppler Lidar and a Sun Photometer X. Wang et al. 10.3390/rs13163259
- The investigation of retrieval method for aerosol and water vapor profiles based on MAX-DOAS technology C. Zhou et al. 10.1016/j.apr.2024.102183
- Shipborne Wind Measurement and Motion-induced Error Correction of a Coherent Doppler Lidar over the Yellow Sea in 2014 X. Zhai et al. 10.5194/amt-11-1313-2018
- The Evolution of Springtime Water Vapor Over Beijing Observed by a High Dynamic Raman Lidar System: Case Studies T. Su et al. 10.1109/JSTARS.2017.2653811
- Investigation of the Spatial and Temporal Variation of Temperature and Water Vapor in Lower Troposphere Using the Combined Backward Raman Scattering LiDAR and Lateral Scanning Raman Scattering LiDAR F. Yang et al. 10.1109/TGRS.2024.3467340
- Raman lidar water vapor profiling over Warsaw, Poland I. Stachlewska et al. 10.1016/j.atmosres.2017.05.004
Saved (final revised paper)
Latest update: 21 Nov 2024
Short summary
The water vapor expedition experiment was operated in the Tibetan Plateau during July and August 2014, by using water vapor, cloud, and aerosol lidar. During the observations, water vapor mixing ratio at high elevation was obtained. The validation of water vapor mixing ratio was completed by comparing the lidar measurements to radiosonde data. Finally, with the vertical wind speed, the vertical flux of water vapor is calculated and the upwelling and deposition of the water vapor are monitored.
The water vapor expedition experiment was operated in the Tibetan Plateau during July and August...