๐”– Bobbio Scriptorium
โœฆ   LIBER   โœฆ

Spectra and cross-spectra of velocity components in the mesometeorological range

โœ Scribed by H. A. Panofsky; I. van der Hoven

Publisher
John Wiley and Sons
Year
1955
Tongue
English
Weight
262 KB
Volume
81
Category
Article
ISSN
0035-9009

No coin nor oath required. For personal study only.

โœฆ Synopsis

Abstract

Power spectra of horizontal wind components at 91 m indicate the existence of a gap near wavelengths of the order of 10 km or periods of the order of one hour.

๐Ÿ“œ SIMILAR VOLUMES

Vertical cross-spectra of horizontal vel
Vertical cross-spectra of horizontal velocity components at the Boulder observatory
โœ Rick Soucy; Robert Woodward; H. A. Panofsky ๐Ÿ“‚ Article ๐Ÿ“… 1982 ๐Ÿ› Springer ๐ŸŒ English โš– 555 KB

Cross-spectra between horizontal wind components at different levels ofthe Boulder Atmospheric Observatory (BAO) tower lead to the following conclusions: (1) Davenport's hypothesis is satisfied that coherence decays exponentially with the ratio of vertical separation to horizontal wave length, at l

Spectra of velocity components over comp
Spectra of velocity components over complex terrain
โœ H. A. Panofsky; D. Larko; R. Lipschutz; G. Stone; E. F. Bradley; A. J. Bowen; J. ๐Ÿ“‚ Article ๐Ÿ“… 1982 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 864 KB
A note on the spectra of wind velocity c
A note on the spectra of wind velocity components in the surface layer
โœ V. Kr. Shรกrรกn; Sture Wickerts ๐Ÿ“‚ Article ๐Ÿ“… 1974 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 305 KB

## Abstract Results of our recent investigation of spectral measurements of wind velocity in the surface layer are analysed in light of the hypothesis proposed by Kaimal __et al.__ (1972). It is confirmed that in the inertial subrange the spectra for all the three components and varying stability c