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A Raman lidar to measure water vapor in the atmospheric boundary layer
Institution:1. Texas Water Resources Institute, Texas A&M University, 1500 Research Parkway A110, College Station, TX 77843-2260, USA;2. Department of Geology and Geophysics, Texas A&M University, College Station, TX 77843-2260, USA;1. LMFA, École Centrale de Lyon, Université de Lyon, CNRS, INSA, UCBL, Écully, France;2. Sorbonne Universités, UPMC Univ. Paris 06, CNRS, UMR 7190, Institut Jean Le Rond d’Alembert, F-75005 Paris, France;3. CEA, DAM, DIF, 91297 Arpajon, France;4. Newport News, VA, USA
Abstract:A new multi-telescope scanning Raman lidar designed to measure the water vapor mixing ratio in the atmospheric boundary layer for a complete diurnal cycle with high resolution spatial (1.25 m) and temporal (1 s) resolutions is presented. The high resolution allows detailed measurements of the lower atmosphere and offers new opportunities for evaporation and boundary layer research, atmospheric profiling and visualization. This lidar utilizes a multi-telescope design that provides for an operational range with a nearly constant signal-to-noise ratio, which allows for statistical investigations of atmospheric turbulence. This new generation ground-based water vapor Raman lidar is described, and first observations from the Turbulent Atmospheric Boundary Layer Experiment (TABLE) are presented. Direct comparison with in-situ point measurements obtained during the field campaign demonstrate the ability of the lidar to reliably measure the water vapor mixing ratio. Horizontal measurements taken with time are used to determine the geometric characteristics of coherent structures. Vertical scans are used to visualize nocturnal jet features, layered structures within a stably stratified atmosphere and the internal boundary layer structure over a lake.
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