Doppler Lidar - Fixed Pointing mode - dlfptThe Doppler lidar (DL) is an active remote-sensing instrument that provides range- and time-resolved measurements of the line-of-sight component of air velocity (i.e., radial velocity) and attenuated aerosol backscatter. The DL operates in the near-infrared and is sensitive to backscatter from atmospheric aerosol, which are assumed to be ideal tracers of atmospheric wind fields. \n \nThe DL works by transmitting short pulses of infrared laser light into the atmosphere. Atmospheric aerosols scatter a small fraction of that light energy back to the transceiver, where it is collected and recorded as a time-resolved signal. From the delay between the outgoing pulse and the backscattered signal, the instrument infers the distance to the scattering volume. \n \nCoherent detection is used to measure the Doppler frequency shift of the backscatter signal. This is accomplished by mixing the backscatter signal with a reference laser beam (i.e., local oscillator) of known frequency. The onboard signal processor then determines the Doppler frequency shift from the spectrum of the mixed signal. The Doppler frequency shift and thus the radial air velocity is determined from the peak of the Doppler spectrum. The attenuated backscatter is determined from the energy content of the Doppler spectra. \n \nThe DL provides accurate measurements of radial velocity in regions of the atmosphere where aerosol concentrations are high enough to ensure good signal-to-noise ratio. Thus, valid data are usually limited to the atmospheric boundary layer where aerosol is ubiquitous. Valid measurements can also be obtained in elevated aerosol layers or in optically thin clouds above the boundary layer. Most of the ARM DLs have full upper-hemispheric scanning capability, enabling 3D mapping of turbulent flows in the atmospheric boundary layer. With the scanner pointed vertically, the DL provides height- and time-resolved measurements of vertical velocity.
Evaluation of turbulence measurement techniques from a single Doppler lidar Atmospheric Measurement TechniquesMeasurements of turbulence are essential to understand and quantify the transport and dispersal of heat, moisture, momentum, and trace gases within the planetary boundary layer (PBL). Through the years, various techniques to measure turbulence using Doppler lidar observations have been proposed. However, the accuracy of these measurements has rarely been validated against trusted in situ instrumentation. Herein, data from the eXperimental Planetary boundary layer Instrumentation Assessment (XPIA) are used to verify Doppler lidar turbulence profiles through comparison with sonic anemometer measurements. For 17 days at the end of the experiment, a single scanning Doppler lidar continuously cycled through different turbulence measurement strategies: velocity-azimuth display (VAD), six-beam scans, and range-height indicators (RHIs) with a vertical stare. Measurements of turbulence kinetic energy (TKE), turbulence intensity, and stress velocity from these techniques are compared with sonic anemometer measurements at six heights on a 300m tower. The six-beam technique is found to generally measure turbulence kinetic energy and turbulence intensity the most accurately at all heights (r(2) approximate to 0.78), showing little bias in its observations (slope of approximate to 0.95). Turbulence measurements from the velocity-azimuth display method tended to be biased low near the surface, as large eddies were not captured by the scan. None of the methods evaluated were able to consistently accurately measure the shear velocity (r(2) = 0.15-0.17). Each of the scanning strategies assessed had its own strengths and limitations that need to be considered when selecting the method used in future experiments.
ULS-BLS Point Cloud Datasets for Forest RegistrationWe collected a test dataset for BLS-ULS registration in an experimental woodland of Northeast Forestry University (129.10°E, 46.90°N). Five representative plots were selected to capture the topographic variation, all representing natural mixed coniferous-broadleaved forests with complex structure and more than ten tree species. ULS data were acquired using a DJI M350 UAV equipped with a GreenValley H800 LiDAR sensor (https://www.greenvalleyintl.com). BLS data were collected using a GreenValley H300 LiDAR sensor.
CLAMPS2 Doppler Lidar VAD DataVAD (Velocity Azimuth Display) observations from the University of Oklahoma/NSSL CLAMPS2 (Collaborative Lower Atmospheric Mobile Profiling System 2) Doppler Lidar that was...
NOAA/ATDD Belle Mina, Alabama Doppler Lidar Radial Velocity Data. Version 1.0This data set contains continuous profiles of radial velocity, speed dispersion, and carrier-to-noise ratio data from the Leosphere WINDCUBE 100s Doppler Lidar that NOAA/ATDD deployed at Belle Mina, Alabama during the VORTEX-SE 2016 field campaign. The profiles typically reliably cover the lowest 2km (occasionally 3km).
Doppler Lidar - Fixed Pointing mode - dlfptThe Doppler lidar (DL) is an active remote-sensing instrument that provides range- and time-resolved measurements of the line-of-sight component of air velocity (i.e., radial velocity) and attenuated aerosol backscatter. The DL operates in the near-infrared and is sensitive to backscatter from atmospheric aerosol, which are assumed to be ideal tracers of atmospheric wind fields. \n \nThe DL works by transmitting short pulses of infrared laser light into the atmosphere. Atmospheric aerosols scatter a small fraction of that light energy back to the transceiver, where it is collected and recorded as a time-resolved signal. From the delay between the outgoing pulse and the backscattered signal, the instrument infers the distance to the scattering volume. \n \nCoherent detection is used to measure the Doppler frequency shift of the backscatter signal. This is accomplished by mixing the backscatter signal with a reference laser beam (i.e., local oscillator) of known frequency. The onboard signal processor then determines the Doppler frequency shift from the spectrum of the mixed signal. The Doppler frequency shift and thus the radial air velocity is determined from the peak of the Doppler spectrum. The attenuated backscatter is determined from the energy content of the Doppler spectra. \n \nThe DL provides accurate measurements of radial velocity in regions of the atmosphere where aerosol concentrations are high enough to ensure good signal-to-noise ratio. Thus, valid data are usually limited to the atmospheric boundary layer where aerosol is ubiquitous. Valid measurements can also be obtained in elevated aerosol layers or in optically thin clouds above the boundary layer. Most of the ARM DLs have full upper-hemispheric scanning capability, enabling 3D mapping of turbulent flows in the atmospheric boundary layer. With the scanner pointed vertically, the DL provides height- and time-resolved measurements of vertical velocity.
NSSL Mobile Lidar Truck Doppler Lidar DataVAD (Velocity Azimuth Display) and vertical stare observations from the NSSL Mobile Lidar Truck Doppler Lidar that was deployed at locations around the southeast United States...
UNR Doppler lidar dataUniversity of Nevada, Reno Doppler lidar data files during Langdon Mountain Prescribed Fire on November 7th 2019
CLAMPS1 Doppler Lidar Vertical Stare DataVertical stare observations from the University of Oklahoma/NSSL CLAMPS1 (Collaborative Lower Atmospheric Mobile Profiling System 1) Doppler Lidar that was deployed at Lake...
CLAMPS1 Doppler Lidar VAD DataThese files contain 24 hour periods of data collected from the CLAMPS1 Halo Streamline XR Doppler lidar. The Doppler lidar conducts regular conical scans at a set elevation...