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Study of the quasi-two-day wave during summer over Santa Maria, Brazil using meteor radar observations

机译:使用流星雷达观测技术研究巴西圣玛丽亚夏季夏季的两天波

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摘要

Characteristics of the quasi-two-day wave (QTDW) have been investigated during late summer of 2005, 2006 and 2007 using meteor wind observations over Santa Maria (29.7°S, 53.7°W), Brazil. Significant inter-annual variability is evident in the derived wave parameters. Maximum wave amplitude is found to be 18 and 42. m/s for zonal and meridional wind, respectively. Mean vertical wavelength shows the values of ~62 and 74. km for zonal and meridional components, respectively. In general high QTDW amplitude is observed when diurnal tide amplitude is lower suggesting strong wave-tide interaction and enhancement of the QTDW at the expense of the diurnal tide energy. Furthermore, the amplitude of the QTDW reveals a clear modulation of 7-8 days periodicity suggesting nonlinear interaction among planetary waves and a probable reason for the observed QTDW variability. Comparison of the present site with the other two Brazilian low latitude sites reveals overall latitudinal invariance except during a few local and/or transient events. There is an indication of wave ducting in the mesosphere and lower thermosphere through which the QTDW can extend latitudinally. Although the response of the QTDW to the mean background wind sometimes exhibits meridional (northward) acceleration, there is no evident signature in the zonal background wind. Both mechanisms suggested so far for exciting the QTDW, i.e. (i) baroclinic/barotropic instability and (ii) Rossby-gravity normal modes are found to be consistent with the present findings.
机译:利用巴西圣玛丽亚(29.7°S,53.7°W)上的流星风观测资料,研究了2005年,2006年和2007年夏末的准两日波(QTDW)特征。在导出的波浪参数中,明显的年际变化。发现纬向风和子午风的最大波幅分别为18和42. m / s。平均垂直波长分别显示纬向和经向分量的〜62和74. km值。通常,当日潮幅值较低时,会观察到较高的QTDW幅值,表明强潮汐作用和QTDW增强,但以日潮能为代价。此外,QTDW的振幅揭示了7-8天周期的明确调制,表明行星波之间存在非线性相互作用,并且是观测到的QTDW变异性的可能原因。本站点与其他两个巴西低纬度站点的比较表明,除了少数局部和/或短暂事件外,整个纬度不变。有迹象表明在中层和下层热层存在波导管,QTDW可以横向延伸。尽管QTDW对平均背景风的响应有时表现为子午(向北)加速度,但纬向背景风中没有明显的特征。迄今为止,两种机制都被认为是激发QTDW的机制,即(i)斜压/正压不稳定性和(ii)Rossby重力正态模式与本研究结果一致。

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