Abstract:
Zonal empirical model of stratosphere fundamental
parameter variation is introduced. The model is based upon diurnal
UK Met Office data on geopotential heights, temperature, zonal and
meridional winds for 1992–2005 period both for northern and
southern hemispheres. Dispersions calculated using the scatter in
average time values and in average zonal values were used as
variability measure.
Analysis reveals that both time and space variabilities of each
parameter have individual features that accord to physics of
global circulation in atmosphere (troposphere and stratosphere).
Quantitative prevalence of non-stationary processes in the upper
atmosphere as related to the lower atmosphere was described.
Discovered features of the stratosphere fundamental parameter
fields' variability may serve as a base for a new reference model
of the mid atmosphere at heights 10–55 km
Keywords:middle atmosphere, variability of thermodynamical fields, reference atmosphere.