1992
DOI: 10.1016/0021-9169(92)90059-t
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Mesosphere and lower thermosphere (80–120 km) winds and tides from near Troms0 (70°N, 19°E) : comparisons between radars (MF, EISCAT, VHF) and rockets

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Cited by 47 publications
(38 citation statements)
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“…The model produces only weak winds at the same height and time of the year. These summer equatorward motions have also been observed at other high latitude stations, for example, Heiss Island, Molodezhnaya, Tromsø, and Scott Base (Lysenko et al, 1979;Fraser, 1984;Manson et al, 1992). The maximum amplitude of southward winds in the observation and model is 12-16 m/s and the corresponding northward wind amplitude is only 4 m/s.…”
Section: Mean Windssupporting
confidence: 73%
“…The model produces only weak winds at the same height and time of the year. These summer equatorward motions have also been observed at other high latitude stations, for example, Heiss Island, Molodezhnaya, Tromsø, and Scott Base (Lysenko et al, 1979;Fraser, 1984;Manson et al, 1992). The maximum amplitude of southward winds in the observation and model is 12-16 m/s and the corresponding northward wind amplitude is only 4 m/s.…”
Section: Mean Windssupporting
confidence: 73%
“…Examples of comparisons include an MFR and Meteor Wind Radar (MWR) at 43 • N ; MFRs and Fabry-Perot Interferometers ("green line" and hydroxyl) at two 52N locations Meek et al, 1997); and rockets and radars (MFR, VHF and EISCAT) near 70 • N (Manson et al, 1992). In these studies the directions of the winds or their perturbations (tidal phases) have been satisfactorily consistent, i.e.…”
Section: Radarsmentioning
confidence: 89%
“…To sort out such rather subtle effects from the background E-region neutral wind, it is important to establish the neutral wind pattern for the quiet E-region. This is the background for recent studies of the E-region neutral wind by Johnson et al (1987), Williams and Virdi (1989), Manson et al (1990Manson et al ( , 1992, Kunitake and Schlegel (1991) and Brekke et al (1994).…”
mentioning
confidence: 86%
“…In recent years data obtained by the advanced EISCAT (European Incoherent Scatter) facility located at Tromso, Norway (69.6°N,19.2°E, A = 66.3°) (Folkestad et al, 1983) has been used by several authors to derive the auroral E-region neutral wind for different geomagnetic conditions (Williams and Virdi, 1989;Manson et al, 1990Manson et al, , 1992Kunitake and Schlegel, 1991;Virdi and Williams, 1993;Brekke et al, 1994;Nozawa and Brekke, 1995;Kofman et al, 1996).…”
mentioning
confidence: 99%
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