Mean winds of the mesosphere and lower thermosphere at 52° N in the period 1988–2000
A meteor radar in the UK (near 52° N) has been used to measure the mean winds of the mesosphere/lower-thermosphere (MLT) region over the period 1988–2000. The seasonal course and interannual variability is characterised and comparisons are made with a number of models. Annual mean wind trend...
Main Authors: | , , |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2002-01-01
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Series: | Annales Geophysicae |
Online Access: | https://www.ann-geophys.net/20/81/2002/angeo-20-81-2002.pdf |
Summary: | A meteor radar in the UK
(near 52° N) has been used to measure the mean winds of the
mesosphere/lower-thermosphere (MLT) region over the period 1988–2000. The
seasonal course and interannual variability is characterised and comparisons
are made with a number of models. Annual mean wind trends were found to be +
0.37 ms<sup>-1</sup> yr<sup>-1</sup> for the zonal component and + 0.157 ms<sup>-1</sup>
yr<sup>-1</sup> for the meridional component. Seasonal means revealed
significant trends in the case of meridional winds in spring ( + 0.38 ms<sup>-1</sup>
yr<sup>-1</sup>) and autumn ( + 0.29 ms<sup>-1</sup> yr<sup>-1</sup>), and
zonal winds in summer ( + 0.48 ms<sup>-1</sup> yr<sup>-1</sup>) and autumn ( +
0.38 ms<sup>-1</sup> yr<sup>-1</sup>). Significant correlation coefficients, <i>R</i>,
between the sunspot number and seasonal mean wind are found in four instances.
In the case of the summer zonal winds, <i>R</i> = + 0.732; for the winter
meridional winds, <i>R </i>= - 0.677; for the winter zonal winds, <i>R</i> = -
0.472; and for the autumn zonal winds <i>R</i> = + 0.508.<br><br><b>Key words. </b>Meteorology and
atmospheric dynamics (climatology; general circulation; middle atmospheric
dynamics) |
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ISSN: | 0992-7689 1432-0576 |