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Time-variability of the ionospheric electric field: solar wind driving and atmospheric feedback

电离层电场的时变性：太阳风驱动和大气反馈

基本信息

批准号：
NE/P001556/1
负责人：
Adrian Grocott
金额：
$ 51.4万
依托单位：
Lancaster University
依托单位国家：
英国
项目类别：
Research Grant
财政年份：
2016
资助国家：
英国
起止时间：
2016 至无数据
项目状态：
已结题

来源：
https://gtr.ukri.org/projects?ref=NE%2FP001556%2F1
关键词：
Time variability ionospheric electric field

项目摘要

The Earth's atmosphere is a complex system consisting of many layers that interact in controlling its global dynamics. The ionosphere plays a key role in these dynamics, coupling the magnetic environment of geospace - 'the magnetosphere' - above to the neutral environment below. Variability in the coupling of electromagnetic fields and particles between Earth's atmosphere and space are responsible for the phenomenon of 'space weather'. This is recognised by current NERC strategy as an environmental hazard with serious global impacts, but limitations in our understanding of its effects on the atmosphere constrain our prediction capability. Ionospheric electric fields, in particular, play an important role in governing atmospheric dynamics, primarily in the thermosphere below 150 km. This is demonstrated by the UK Met Office seeking to include the thermosphere in their weather and climate model, raising the upper boundary of its Unified Model (MetUM) from 85 km to the region of 120-140 km. In order to achieve this, improved ionospheric electric field models are essential, since existing models characterise only average conditions and have no 'memory' of the prior history of variability. Capturing this variability is critical if realistic predictions of atmospheric dynamics are to be made at these altitudes. We will therefore develop the next generation model of global ionospheric electric fields that will include, for the first time, the inherent time-dependence of their morphology and driving mechanisms. Specifically, we include variability associated with three distinct sources: (i) solar wind driving (ii) dynamical processes in geospace and (iii) atmospheric feedback. Our model will be designed in collaboration with the UK Met Office, for use in their climate and space weather modelling applications such as MetUM.To achieve our goals we will utilise multi-decadal datasets of electric and magnetic field measurements from ionospheric radars and ground magnetometers, and neutral wind measurements by Fabry-Perot interferometers, to study the electrodynamics of the ionosphere, and its coupling to the neutral atmosphere. We will use upstream interplanetary spacecraft data to order our observations not only by the concurrent conditions in geospace, but by the time history of these conditions; persistent plasma and magnetic field structures, and the degree of variability. We will also use geomagnetic measurements to investigate the effects of time-variable internal magnetospheric processes. These include magnetospheric substorms, which excite convection in the ionosphere, inject energetic particles into the atmosphere, and produce the visible aurora, or northern (and southern) lights. Lastly, we will use simultaneous measurements of the electric field and neutral wind to investigate the 'flywheel' effect of the neutral wind dynamo; the ability of neutral winds to maintain the ionospheric electric field after their direct excitation subsides. Incorporating all of these time-variable effects into a new empirical model of the ionospheric electric field will provide a valuable resource for magnetospheric physics, atmospheric modellers, and space plasma physics theorists.

地球大气层是一个复杂的系统，由许多层组成，这些层相互作用，控制着它的全球动力学。电离层在这些动力学中起着关键作用，将地球空间的磁性环境（“磁层”）与上面的中性环境耦合在一起。地球大气和空间之间电磁场和粒子耦合的变异性是造成“空间天气”现象的原因。目前的NERC战略认识到这是一种具有严重全球影响的环境危害，但我们对其对大气影响的理解有限，限制了我们的预测能力。特别是电离层电场，在控制大气动力学方面起着重要作用，主要是在150公里以下的热层。英国气象局试图将热层纳入他们的天气和气候模型，将其统一模型（MetUM）的上边界从85公里提高到120-140公里，就证明了这一点。为了实现这一点，改进的电离层电场模型是必不可少的，因为现有的模型只描述平均条件，没有对以前变率历史的“记忆”。如果要在这些高度对大气动力学作出现实的预测，捕捉这种变化是至关重要的。因此，我们将开发下一代全球电离层电场模型，该模型将首次包括其形态和驱动机制的固有时间依赖性。具体来说，我们包括与三个不同来源相关的变率：(i)太阳风驱动（ii）地球空间动力学过程和（iii）大气反馈。我们的模型将与英国气象局合作设计，用于他们的气候和空间天气建模应用程序，如MetUM。为了实现我们的目标，我们将利用电离层雷达和地面磁力计的多年电场和磁场测量数据集，以及Fabry-Perot干涉仪的中性风测量数据，研究电离层的电动力学及其与中性大气的耦合。我们将利用上游行星际航天器的数据，不仅根据地球空间的同步条件，而且根据这些条件的时间历史来安排我们的观测；持续的等离子体和磁场结构，以及变异性的程度。我们还将使用地磁测量来研究随时间变化的内部磁层过程的影响。这些包括磁层亚暴，它激发电离层的对流，向大气中注入高能粒子，并产生可见的极光，或北极光（和南极光）。最后，我们将使用电场和中性风的同时测量来研究中性风力发电机的“飞轮”效应；中性风在其直接激励消退后维持电离层电场的能力。将所有这些时变效应整合到电离层电场的新经验模型中，将为磁层物理学、大气建模者和空间等离子体物理学理论家提供宝贵的资源。