Statistics of wind direction and its increments
Phys. Fluids 12, 1529 (2000); doi:10.1063/1.870401
Issue Date: June 2000
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We study some elementary statistics of wind direction fluctuations in the atmosphere for a wide range of time scales (104 sec to 1 h), and in both vertical and horizontal planes. In the plane parallel to the ground surface, the direction time series consists of two parts: a constant drift due to large weather systems moving with the mean wind speed, and fluctuations about this drift. The statistics of the direction fluctuations show a rough similarity to Brownian motion but depend, in detail, on the wind speed. This dependence manifests itself quite clearly in the statistics of wind-direction increments over various intervals of time. These increments are intermittent during periods of low wind speeds but Gaussian-like during periods of high wind speeds. ©2000 American Institute of Physics.
| History: | Received 26 March 1999; accepted 6 March 2000 |
| Permalink: |
http://link.aip.org/link/?PHFLE6/12/1529/1 |
KEYWORDS and PACS
WIND,
STATISTICAL DATA,
FLUCTUATIONS,
EARTH ATMOSPHERE,
BROWNIAN MOVEMENT,
VELOCITY,
statistical analysis,
time series,
Brownian motion
- 92.60.Gn
Hydrospheric and atmospheric geophysics Meteorology Winds and their effects - 05.40.Jc
Statistical physics, thermodynamics, and nonlinear dynamical systems Fluctuation phenomena, random processes, noise, and Brownian motion Brownian motion - 02.50.-r
Mathematical methods in physics Probability theory, stochastic processes, and statistics - YEAR: 2000
PUBLICATION DATA
1070-6631 (print)
1089-7666 (online)
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