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In situ observations of waves in Venus's polar lower thermosphere with Venus Express aerobraking

机译:利用Venus Express气动制动技术对金星极地下部热圈中的波进行原位观测

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Waves are ubiquitous phenomena found in oceans and atmospheres alike. From the earliest formal studies of waves in the Earth's atmosphere to more recent studies on other planets, waves have been shown to play a key role in shaping atmospheric bulk structure, dynamics and variability(1-4). Yet, waves are difficult to characterize as they ideally require in situ measurements of atmospheric properties that are difficult to obtain away from Earth. Thus, we have incomplete knowledge of atmospheric waves on planets other than our own, and we are thereby limited in our ability to understand and predict planetary atmospheres. Here we report the first ever in situ observations of atmospheric waves in Venus's thermosphere (130-140 km) at high latitudes (71.5 degrees-79.0 degrees). These measurements were made by the Venus Express Atmospheric Drag Experiment (VExADE)(5) during aerobraking from 24 June to 11 July 2014. As the spacecraft flew through Venus's atmosphere, deceleration by atmospheric drag was sufficient to obtain from accelerometer readings a total of 18 vertical density profiles. We infer an average temperature of T = 114 +/- 23 K and find horizontal wave-like density perturbations and mean temperatures being modulated at a quasi-5-day period.
机译:波浪是在海洋和大气中普遍存在的现象。从最早的对地球大气中波的形式化研究到对其他行星的最新研究,波被证明在塑造大气体结构,动力学和可变性方面起着关键作用(1-4)。然而,由于很难对海浪进行表征,因为它们理想地需要对从地球上很难获得的大气特性进行原位测量。因此,我们对除自己之外的行星上的大气波了解不全,因此我们在理解和预测行星大气方面的能力受到限制。在这里,我们报告在高纬度(71.5度至79.0度)的金星热圈(130-140公里)中首次对大气波进行原位观测。这些测量是由维纳斯快速大气阻力实验(VExADE)(5)在2014年6月24日至7月11日的航空制动过程中进行的。随着航天器飞越维纳斯大气层,大气阻力引起的减速度足以从加速度计读数中获得总计18垂直密度剖面。我们推断出平均温度为T = 114 +/- 23 K,发现水平波状密度扰动和平均温度在准5天周期内被调制。

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