In:
Radio Science, American Geophysical Union (AGU), Vol. 4, No. 12 ( 1969-12), p. 1257-1259
Abstract:
A joint experiment using Doppler radar technique and instrumented aircraft has produced comparative measurements of wind‐speed fluctuations under convective conditions in the lowest 500 meters. Preliminary results show a good agreement between radar and aircraft spectra of a longitudinal wind‐speed component at scales from 50 meters to 1 km. There is an indication that, at scales larger than 1 km, Taylor's hypothesis is not valid.
Type of Medium:
Online Resource
ISSN:
0048-6604
,
1944-799X
DOI:
10.1029/RS004i012p01257
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
1969
detail.hit.zdb_id:
2011445-X
SSG:
16,13
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