首页> 外文期刊>Journal of atmospheric and solar-terrestrial physics >Planetary waves observed by TIMED/SABER in coupling the stratosphere-mesosphere-lower thermosphere during the winter of 2003/2004: Part 2-Altitude and latitude planetary wave structure
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Planetary waves observed by TIMED/SABER in coupling the stratosphere-mesosphere-lower thermosphere during the winter of 2003/2004: Part 2-Altitude and latitude planetary wave structure

机译:TIMED / SABRE在2003/2004年冬季观测到的平流层-中层-低层热层耦合中的行星波:第2部分:海拔和纬度行星波结构

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Part 2 of the present paper is focused on the planetary wave coupling from the stratosphere to the lower thermosphere (30-120 km) during the Arctic winter of 2003/2004. The planetary waves seen in the TIMED/SABER temperature data in the latitudinal range 50 degrees N-50 degrees S are studied in detail. The altitude and latitude structures of the planetary wave (stationary and travelling) clearly indicate that the stratosphere and mesosphere (30-90 km) are coupled by direct vertical propagation of the planetary waves, while the lower thermosphere (above 90-95km altitude) is only partly connected with the lower levels probably indirectly through in-situ generation of disturbances by the dissipation and breaking of gravity waves filtered by lower atmospheric planetary waves. A peculiar feature of the thermal regime in the lower thermosphere is that it is dominated by zonally symmetric planetary waves.
机译:本文的第2部分着重于2003/2004北极冬季从平流层到低热层(30-120 km)的行星波耦合。详细研究了TIMED / SABER温度数据中纬度范围为50度N-50度S的行星波。行星波的高度和纬度结构(平稳的和行进的)清楚地表明,平流层和中层层(30-90 km)是由行星波的直接垂直传播耦合的,而下部热层(海拔90-95 km以上)是通过与低层大气行星波滤除的重力波的消散和破坏,原地产生干扰,从而间接地间接地与低层部分相连。下部热圈中热态的一个独特特征是,它以纬向对称的行星波为主。

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