The Impact of Energetic Neutral Particles Raining Down on the Thermosphere due to Charge Exchange Reactions in the Upper Ionosphere and Polar Wind

由于电离层上部和极地风的电荷交换反应，高能中性粒子雨落到热层上的影响

• 批准号: 1834894
• 负责人: Larry Gardner
• 金额: $ 32.28万
• 依托单位: Utah State University
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2019
• 资助国家: 美国
• 起止时间: 2019-07-15 至 2024-06-30
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1834894&HistoricalAwards=false
• 关键词: Impact; Energetic; Neutral; Particles; Raining

The upper atmosphere in the polar regions contains a layer of weakly ionized gas (the ionosphere). Ionized particles such as hydrogen and oxygen ions drift upward in response to heating via electric fields and particle precipitation from the near-Earth space and can reach velocities as high as 10-20 km/s for hydrogen and 3-5 km/s for oxygen. These energetic ions interact with surrounding neutral gas (the thermosphere) and energetic neutral atoms are produced in charge exchange reactions. Light hydrogen atoms escape the atmosphere but heavy neutral species such as oxygen cannot escape and reverse direction. In the polar cap ionosphere-thermosphere system, this gives rise to a continuous Polar Rain. This award will investigate how the energetic neutrals affect circulation, temperature, density, and wave activity in the coupled ionosphere-thermosphere system. The research will contribute to the community effort of modeling of space plasma disturbances by including previously unincluded effects of the energetic neutral particles and by providing a better specification of the required model resolutions. The project will also support a graduate student and contribute to creating a diverse workforce. The work will involve (1) inclusion of new terms in the fluid equations to account for additional types of the ion-neutral and neutral-neutral coupling that are currently not considered, including thermal loss due the energetic atom cooling due to collisions with background neutrals, (2) running a comprehensive set of simulations using the coupled models for various conditions, and (3) investigating effects of different disturbance types.This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.

极地地区的高层大气包含一层弱电离气体(电离层)。氢离子和氧离子等电离粒子在电场加热和近地空间粒子降水的作用下向上漂移，氢气的速度可达10-20公里/S，氧气的速度可达3-5公里/S。这些高能离子与周围的中性气体(热层)相互作用，在电荷交换反应中产生高能中性原子。轻氢原子逃离大气层，但重中性物质，如氧，无法逃逸并逆转方向。在极冠电离层-热层系统中，这导致了持续的极地雨。这一奖项将研究高能中性如何影响电离层-热层耦合系统中的环流、温度、密度和波活动。这项研究将包括以前未包括的高能中性粒子的影响，并更好地说明所需的模型分辨率，从而对空间等离子体扰动的建模工作作出贡献。该项目还将支持一名研究生，并为创建一支多元化的劳动力队伍做出贡献。这项工作将涉及(1)在流体方程中加入新的术语，以说明目前尚未考虑的其他类型的离子-中性和中性-中性耦合，包括由于与背景中性的碰撞导致高能原子冷却而造成的热损失，(2)使用耦合模型对各种条件进行全面的模拟，以及(3)调查不同扰动类型的影响。该奖项反映了NSF的法定使命，并通过使用基金会的智力优势和更广泛的影响审查标准进行评估，被认为值得支持。