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Title: NANT Site - Radar Wind Profiler / Derived Data Reformatted

Abstract

A radar wind profiler measures the Doppler shift of electromagnetic energy scattered back from atmospheric turbulence and hydrometeors along 3-5 vertical and off-vertical point beam directions. Back-scattered signal strength and radial-component velocities are remotely sensed along all beam directions and combined to derive the horizontal wind field over the radar. These data are typically sampled and averaged hourly or sub-hourly (15-min) and usually have 60-m and/or 100-m vertical resolutions up to 4 km for the 915 MHz system. Both a high-resolution, lower height coverage mode and a low-resolution, higher height coverage mode are used to collect the data.

Authors:
; ; ; ;
  1. CIRES
  2. CIRES/NOAA
  3. NOAA
Publication Date:
DOE Contract Number:  
AC05-76RL01830
Research Org.:
Pacific Northwest National Laboratory
Sponsoring Org.:
USDOE Office of Energy Efficiency and Renewable Energy (EERE), Wind and Water Technologies Office (EE-4W)
Subject:
17 WIND ENERGY
OSTI Identifier:
2569390
DOI:
https://doi.org/10.21947/2569390

Citation Formats

Bianco, Laura, Adler, Bianca, Costa, Dave, Osborn, Jackson, and Counts, Kevin. NANT Site - Radar Wind Profiler / Derived Data Reformatted. United States: N. p., 2025. Web. doi:10.21947/2569390.
Bianco, Laura, Adler, Bianca, Costa, Dave, Osborn, Jackson, & Counts, Kevin. NANT Site - Radar Wind Profiler / Derived Data Reformatted. United States. doi:https://doi.org/10.21947/2569390
Bianco, Laura, Adler, Bianca, Costa, Dave, Osborn, Jackson, and Counts, Kevin. 2025. "NANT Site - Radar Wind Profiler / Derived Data Reformatted". United States. doi:https://doi.org/10.21947/2569390. https://www.osti.gov/servlets/purl/2569390. Pub date:Mon Nov 24 04:00:00 UTC 2025
@article{osti_2569390,
title = {NANT Site - Radar Wind Profiler / Derived Data Reformatted},
author = {Bianco, Laura and Adler, Bianca and Costa, Dave and Osborn, Jackson and Counts, Kevin},
abstractNote = {A radar wind profiler measures the Doppler shift of electromagnetic energy scattered back from atmospheric turbulence and hydrometeors along 3-5 vertical and off-vertical point beam directions. Back-scattered signal strength and radial-component velocities are remotely sensed along all beam directions and combined to derive the horizontal wind field over the radar. These data are typically sampled and averaged hourly or sub-hourly (15-min) and usually have 60-m and/or 100-m vertical resolutions up to 4 km for the 915 MHz system. Both a high-resolution, lower height coverage mode and a low-resolution, higher height coverage mode are used to collect the data.},
doi = {10.21947/2569390},
journal = {},
number = ,
volume = ,
place = {United States},
year = {Mon Nov 24 04:00:00 UTC 2025},
month = {Mon Nov 24 04:00:00 UTC 2025}
}