We use cookies to make our websites more user-friendly and to continuously improve them. If you continue to use the website, you consent to the use of cookies. You can find more information in our privacy statement and our cookie guidelines.

To our valued customers,

At last: 

Beuth Verlag is now DIN Media. 

You can find out more about our new name and the reasons behind it here.

To use our new website without any hiccups, please clear your browser cache. 

Yours sincerely,

DIN Media

Standards Worldwide
Standards Worldwide
Phone +49 30 58885700-07

Draft standard [WITHDRAWN]

DIN ISO 23032:2020-10 - Draft

Meteorology - Ground-based remote sensing of wind - Radar wind profiler (ISO/DIS 23032:2020); Text in German and English

German title
Meteorologie - Bodengebundene Fernmessung von Wind - Windprofilmessradar (ISO/DIS 23032:2020); Text Deutsch und Englisch
Date of issue
2020-08-28
Publication date
2020-10
Original language
German, English
Pages
215
Note
The publisher recommends this document in lieu of the withdrawn document VDI 3786 Blatt 17:2007-02 , for which no replacement is available.

Please select

from 216.10 EUR VAT included

from 201.96 EUR VAT excluded

Purchasing options

PDF download 1

  • 216.10 EUR

Shipment (3-5 working days) 1

  • 261.40 EUR

1

 Attention: Document withdrawn!

Date of issue
2020-08-28
Publication date
2020-10
Original language
German, English
Pages
215
Note
The publisher recommends this document in lieu of the withdrawn document VDI 3786 Blatt 17:2007-02 , for which no replacement is available.
DOI
https://dx.doi.org/10.31030/3193592

Product information on this site:

Quick delivery via download or delivery service

Buy securely with a credit card or pay upon receipt of invoice

All transactions are encrypted

Short description
Radar wind profiler, also referred to as wind profiler radar, wind profiling radar, atmospheric radar, or clear-air Doppler radar (hereafter abbreviated to WPR) is an instrument that measures height profiles of wind velocity in clear air. WPR detects echoes produced by perturbations of the radio refractive index with a scale half of the radar wavelength (i.e., Bragg scale). The mechanism of radio wave scattering in clear air was theoretically and experimentally understood in the 1960s. Since the 1970s, large-sized Doppler radars for observing wind and turbulence in the mesosphere, stratosphere, and the troposphere (MST radars) have been developed. Owing to their capability of measuring wind and turbulence with excellent time and height resolution, they have made great contributions to describing and clarifying the dynamical processes in the atmosphere.
Content
ICS
07.060
DOI
https://dx.doi.org/10.31030/3193592

Cooperation at DIN

Also available in
Loading recommended items...
Loading recommended items...
Loading recommended items...
Loading recommended items...