Articles | Volume 36, issue 2
https://doi.org/10.5194/angeo-36-577-2018
https://doi.org/10.5194/angeo-36-577-2018
Regular paper
 | 
03 Apr 2018
Regular paper |  | 03 Apr 2018

High-resolution vertical velocities and their power spectrum observed with the MAARSY radar – Part 1: frequency spectrum

Qiang Li, Markus Rapp, Gunter Stober, and Ralph Latteck

Viewed

Total article views: 1,723 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,184 485 54 1,723 57 48
  • HTML: 1,184
  • PDF: 485
  • XML: 54
  • Total: 1,723
  • BibTeX: 57
  • EndNote: 48
Views and downloads (calculated since 03 Apr 2018)
Cumulative views and downloads (calculated since 03 Apr 2018)

Cited

Latest update: 15 Apr 2024
Download
Short summary
With the powerful MAARSY radar, we detected 3D wind fields and the vertical winds show a non-Gaussian distribution. We further obtained the frequency spectrum of vertical wind. The distribution of the spectral slopes under different wind conditions is derived and their comparisons with the background horizontal winds show that the spectra become steeper with increasing wind velocities under quiet conditions, approach a slope of −5/3 at 10 m/s and then maintain this slope for even stronger winds.