Showing papers by "Iain M. Reid published in 1989"

VHF radar echoes observed in the summer and winter polar mesosphere over Andøya, Norway

Abstract: The mobile SOUSY VHF (53.5 MHz) Radar has been operated on a campaign basis on the island of Andoya in Northern Norway (69°17′N, 16°01′E), with the aim of investigating the backseattering structures and dynamics of the polar middle atmosphere, since November 1983. During winter the occurrence of mesospheric echoes at altitudes from 50 to 90 km is strongly correlated with radio wave absorption events measured with a riometer on 32.5 MHz. Individual structures are observed for up to 8 hours and, in general, appear as thin layers separated by 3–5 km, with typical maximum signal-to-noise ratios (SNRs) of 5–25 dB. Many of these are related to variations in the background wind produced by long-period gravity waves and tidal period motions and, in as much, are similar to mesospheric layers at middle and low latitudes. In summer the echo region is largely restricted to a height interval from 75 to 95 km, with 80% of the echoes occurring in the 80- to 93-km height range, and on average, it has a distinct maximum in SNR near 86 km. In the 83- to 91-km height region, echoes are detected almost continuously, with a minimum occurrence rate of 85%. There is a low correlation (∼0.26) between echo strength and absorption. Many of the weaker echoing regions, those with SNRs up to 30 dB, are related to the background wind shear. Spectral analysis of time series of both SNR and zonal velocity for a period of 9 days reveals 54-, 24-, 12-, and 8-hour components, with the 12-hour component dominating. Strong bursts in backscattered power tend to occur in the late afternoon and early morning hours, so they coincide with the time of maximum westward velocity of the semidiurnal tide. This suggests that the bursts are due to an increase in the turbulent intensity produced by dynamical instability of this mode. Layers consistent with dynamically unstable upward propagating inertio-gravity waves are also often observed to move down through the 93- to 80-km height range. Thus dynamical instability of the semidiurnal tide and long-period gravity waves appears to play a major role in determining much of the structure observed in the backscatter region. However, the strongest summer polar mesopause echoes, those with peak SNRs greater than 30 dB, while showing modulation due to the background winds, often show no clear relation to the background wind shear. This supports the view that the production mechanism of the very strong SNRs associated with this layer is different in character from that of winter echoes observed in the polar mesosphere by VHF radars, and to those mesospheric layers observed at mid-latitudes using the same technique.

First VHF radar measurements of mesopause summer echoes at mid‐latitudes

Abstract: Observations of the summer mesosphere using the stationary SOUSY VHF (535 MHz) radar located in the Harz mountains of Germany (52°N, 10°E) indicate the presence of very strong radar returns from heights near 85–86 km on some occasions These echoes occur in the form of a layer with a full-power half-width of less than about 1 km, and exhibit an aspect sensitivity of about 1 dB deg−1 These features are very similar to those of the so-called Polar Mesopause Summer Echo (PMSE) known to occur at high latitudes and suggest a common production mechanism

VHF radar measurements in the summer polar mesosphere

Abstract: Measurements in the mesosphere over Andoya/Norway (69 N, 16 E) were carried out using the mobile SOUSY-VHF radar with an extended beam configuration during the MAC/SINE campaign in summer 1987. First results of a 48 h and a 3 h observational period for heights between about 83 and 91 km are presented. Zonal mean winds are characterized by a strong westward flow of up to 50/ms, whereas the equatorward directed meridional component is weaker. The dominating semidiurnal tide has amplitudes up to 30/ms and a vertical wavelength of about 55 km. The diurnal tide is less pronounced. The total upward flux of horizontal momentum takes values of -2 sq m/sq s near 84 km and increases with increasing height, reaching a maximum value of 22 sq m/sqs for both the zonal and meridional components. However, measurements of the horizontal isotropy of the wave field suggest significant anisotropy. The major contribution to the momentum flux is from the 10 min to 1 h period range below about 87 km, and from the 1 to 6 h period range above this height.