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High-latitude thermospheric zonal winds during low solar activity period

机译:低太阳活动期间的高纬度热层带风

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Changes resulting from the cyclical nature of the sun’s energy output result to variations in thermosphere-ionosphere system parameters. The prolonged low solar activity period of solar cycle 23 provides an opportunity to study the thermosphere-ionosphere system parameters when the sun was at its ground state. The CHAMP satellite has provided wind data that can be used for investigation of neutral thermospheric parameters such as zonal winds and density. Using zonal wind data from 2006 to 2008 generated from CHAMP accelerometer readings using an iterative algorithm, the diurnal variation of averaged zonal thermospheric winds in the high latitudes (70 - 80°N) has been investigated. In the analysis we grouped the data into four seasons; the March and September equinoxes, and the June and December solstices. The wind data is binned into local time bins and averaged to find the hourly mean speeds. The results reveal maximum eastward and westward wind speeds going above 150 m/s for each of the seasons considered. Of particular interest is the observation that despite the expected complex behavior resulting from the expected magnetospheric inputs, the diurnal patterns are similar to those obtained in the mid-latitudes in an earlier study with data from this algorithm. Due to likely errors arising from the longitudinal effects of mixing composite solar times, there is need for simultaneous measurements in the high latitudes.
机译:由于太阳能量输出的周期性而导致的变化导致热球-电离层系统参数的变化。太阳周期23的延长的低太阳活动期为研究太阳处于基态时提供了热球-电离层系统参数的机会。 CHAMP卫星提供的风数据可用于研究中性热圈参数,例如纬向风和密度。使用从CHAMP加速度计读数中使用迭代算法生成的2006年至2008年的纬向风数据,研究了高纬度(70-80°N)的平均纬向热层风的日变化。在分析中,我们将数据分为四个季节。三月和九月的春分点,以及六月和十二月的冬至。风数据被归入本地时间仓,并进行平均以找到每小时的平均速度。结果表明,在考虑的每个季节中,最大的东,西风速都超过150 m / s。特别令人感兴趣的是,观察到尽管预期的磁层输入会产生预期的复杂行为,但其昼夜模式却与早期研究中使用该算法获得的数据在中纬度获得的模式相似。由于混合太阳时的纵向影响可能引起误差,因此需要在高纬度同时进行测量。

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