z-logo
Premium
Experimental determination of mean Doppler‐reflectivity relationship with a vertically pointing Doppler radar
Author(s) -
Pasqualucci F.
Publication year - 1974
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/gl001i006p00249
Subject(s) - doppler effect , radar , doppler radar , geology , altitude (triangle) , reflectivity , optics , remote sensing , scattering , geodesy , physics , mathematics , telecommunications , astronomy , computer science , geometry
A pseudo noise coded continuous wave Doppler radar, operated at a frequency of 35 GHz, was used to measure drop‐size distributions and the mean Doppler for vertical velocitiesv ¯ . The data have been used to determine a relationship between,v ¯and the radar reflectivity factor, Z. 95% of thev ¯experimental data fall within ±0.3 m sec −1 of thev ¯functionv ¯= 2.67 Z 0.095 ( v ¯m sec −1 ). The spread of the data may be attributed to a small contribution of unknown vertical air velocity in the low altitude (15 m to 25 m) scattering region.

This content is not available in your region!

Continue researching here.

Having issues? You can contact us here
Accelerating Research

Address

John Eccles House
Robert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom