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-1 yr-1 for the zonal component and +0.157 ms-1 yr-1 for the meridional component. Seasonal means revealed significant trends in the case of meridional winds in spring (+0.38 ms-1 yr-1) and autumn (+0.29 ms-1 yr-1), and zonal winds in summer (+0.48 ms-1 yr-1) and autumn (+0.38 ms-1 yr-1). Significant correlation coefficients, R, between the sunspot number and seasonal mean wind are found in four instances. In the case of the summer zonal winds, R = +0.732; for the winter meridional winds, R = -0.677; for the winter zonal winds, R = -0.472; and for the autumn zonal winds R = +0.508.
CITATION STYLE
Middleton, H. R., Mitchell, N. J., & Muller, H. G. (2002). Mean winds of the mesosphere and lower thermosphere at 52° N in the period 1988-2000. Annales Geophysicae, 20(1), 81–91. https://doi.org/10.5194/angeo-20-81-2002
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