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Trade-wind variability, southern oscillation and quasi-biennial oscillation

✍ Scribed by E. R. Reiter

Publisher
Springer
Year
1979
Tongue
English
Weight
859 KB
Volume
28
Category
Article
ISSN
1436-5065

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πŸ“œ SIMILAR VOLUMES

A conceptual model relating the quasi-bi
A conceptual model relating the quasi-biennial oscillation and the tropospheric biennial oscillation
✍ Kok Foo Kwan; Azizan Abu Samah πŸ“‚ Article πŸ“… 2003 πŸ› John Wiley and Sons 🌐 English βš– 755 KB

## Abstract A survey of the zonal wind throughout the troposphere and the lower stratosphere near the equator is made for the 41 year period of 1958–98. A similar survey of the 500 hPa geopotential height, sea‐surface temperature (SST) and tropopause height is also made, except that the survey peri

A global analysis of the variability of
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✍ D. G. Dartt; A. D. Belmont πŸ“‚ Article πŸ“… 1970 πŸ› John Wiley and Sons 🌐 English βš– 561 KB

## Abstract Monthly‐mean zonal wind data from approximately 200 rawin stations have been filtered to remove the annual and shorter period variations. Data from 1950–1964 for levels from 700 to 7 mb were analysed. The primary variation is the quasi‐biennial oscillation of the equatorial stratosphere

A quasi-biennial oscillation in the inte
A quasi-biennial oscillation in the intensity of the intra-seasonal oscillation
✍ Ken-Ichi Kuma πŸ“‚ Article πŸ“… 1990 πŸ› John Wiley and Sons 🌐 English βš– 742 KB

## Abstract The interannual and annual variations in the intra‐seasonal oscillation (ISO) are examined using upper air radiosonde data at Singapore. Spectral analysis of the zonal wind using the maximum entropy method (MEM) was made for each season, starting from the autumn of 1960 through to 1985.

Zonal wind quasi-biennial oscillations a
Zonal wind quasi-biennial oscillations at 25–60 km altitude, 1962–69
✍ G. V. Groves πŸ“‚ Article πŸ“… 1973 πŸ› John Wiley and Sons 🌐 English βš– 472 KB

## Abstract Meteorological rocket observations of zonal winds at thirteen sites (or pairs of sites) have been analysed for amplitudes and phases of their quasi‐biennial oscillation. The period of the oscillation was taken to be 32 months because from 1962–69 the period was relatively constant, not