Published September 15, 2025 | Version 1.0.0
Dataset Open

CLAMPS2 Doppler Lidar VADs

  • 1. ROR icon NOAA National Severe Storms Laboratory
  • 2. Cooperative Institute for Severe and High Impact Weather Research and Operations
  • 3. EDMO icon University of Oklahoma

Description

These files contain 24 hour periods of data collected from the CLAMPS2 Halo Streamline XR+ Doppler lidar. The Doppler lidar conducts regular conical scans at a set elevation angle. These data are then passed through a typical VAD algorithm to retrieve horizontal wind speed and direction profiles. These data were collected during the SCALES project.

 

The Halo Streamline XR+ is a commercial platform. The Doppler lidar (DL) is an active remote-sensing instrument that provides range- and time-resolved measurements of radial velocity, attenuated backscatter, and signal-to-noise ratio (SNR). The principle of operation is similar to radar in that pulses of electromagnetic energy (infrared in this case) are transmitted into the atmosphere; the energy scattered back to the transceiver is collected and measured as a time-resolved signal. From the time delay between each outgoing transmitted pulse and the backscattered signal, the distance to the scatterer is inferred. The radial or line-of-sight velocity of the scatterers is determined from the Doppler frequency shift of the backscattered radiation. The DL uses a heterodyne detection technique in which the return signal is mixed with a reference laser beam (i.e., local oscillator) of known frequency. An onboard signal-processing computer then determines the Doppler frequency shift from the power spectra of the heterodyne signal. The energy content of the Doppler spectra can also be used to estimate attenuated backscatter. The DL operates in the near-infrared (IR;1.5 microns) and is sensitive to backscatter from micron-sized aerosols. Aerosols are ubiquitous in the lower troposphere and behave as ideal tracers of atmospheric winds. In contrast to radar, the DL is capable of measuring radial velocities under clear-sky conditions with very good precision – typically ~10 cm/sec (Newsom and Krishnamurthy 2020).  It is important to note that DL scans are fully user configurable, so special attention should be paid to the scan strategy applied for this dataset.

 

Additional documentation available within the dataset as a readme file.

Files

Files (6.5 MB)

Name Size Download all
md5:54867e1732ac2a44c5799f9f7eb7418e
34.3 kB Download
md5:ab44ee16a85dd9245d3920a98e3b5b17
1.5 MB Download
md5:73a69dfd1588fe069f7782ea12de76bc
1.5 MB Download
md5:fd3476901302c7269c93536828016d8b
515.5 kB Download
md5:d76468b6ed65a83010025314d1004c26
1.5 MB Download
md5:1f964c821615c48373a3fdd450c5ff9f
1.5 MB Download

Additional details

Dates

Valid
2024-09-07
Observation period begins
Valid
2024-09-14
Observation period ends
Submitted
2025-09-15
Data submitted