FG: Radiation Belts as a System of Systems

Dates: 2025 – 2029
Leaders: Longzhi Gan, Harriet George, Man Hua, Adam Michael, Luisa Capannolo
Research Areas: Primary – IMAG, Secondary – None

Topic

The science goals that this FG will focus on are:

1. Determine and quantify how radiation belt particle dynamics are controlled by and how they affect systems that couple to the terrestrial radiation belts. This includes phenomena such as the rates of acceleration, transport or loss under different solar wind, geomagnetic storm and substorm conditions, radiation belt precipitation as an input to the atmosphere/ionosphere system, and radiation belt particle dynamics following particle injections from the magnetotail. This inherently includes evaluation of the impact of wave-particle interactions that are modulated by the coupled systems, which are elaborated on in Goal 2.
2. Determine how plasma wave activity within the inner magnetosphere is governed by the coupled systems, and quantify the importance of wave activity to particle dynamics via wave-particle interactions. This includes evaluating the role that coupled systems play on the spatial distribution (including magnetic local time distribution), growth rate and intensity of inner magnetospheric plasma waves. For example, magnetotail injections create particle anisotropies that can lead to plasma wave generation. The plasmapause also acts as a boundary between the growth of whistler-mode chorus and hiss waves. The coupled systems, therefore, play a defining role in the generation and characteristics of inner mag- netospheric waves. Radiation belt wave-particle interactions are further modulated by these coupled systems. The distribution of cold plasma can alter both the efficiency of wave-particle interactions and the spatial extent of the region where the interaction takes place, impacting the particle dynamics that are considered in Goal 1, such as the rates of pitch-angle scattering or acceleration.
3. Evaluate how system-wide radiation belt evolution is modulated by the coupled systems, and the effect that these system-wide dynamics have on the coupled systems. This goal specifically evaluates radiation belt dynamics that persist significantly longer than a drift period (≳ hours/days) and affect the entire radiation belt environment, such as long-term dropouts and enhancements. For example, some geomagnetic storms and substorms drive radiation belt enhancements more efficiently than other storms, so determining the solar wind and/or magnetotail conditions that result in this varying enhancement efficiency is an important aspect of accurate geospace modeling that is encompassed by this FG. This science topic includes determining and quantifying the effects that large-scale radiation belt dynamics have on the coupled systems, such as the impact of particle precipitation during radiation belt dropout events on the atmosphere/ionosphere system.

Evaluation of the influence of the solar wind on the Earth’s radiation belt includes the impact that specific solar wind/IMF parameters have on the radiation belts. The FG additionally includes evaluation of the impact of solar wind transients, such as high speed solar wind streams or coronal mass ejections, on long-term, system-wide radiation belt enhancements or dropouts, and variations in the radiation belts on solar-cycle timescales that result from changing solar wind/IMF conditions throughout the solar cycle.

The coupling of the magnetotail to the radiation belts includes evaluation of the impact of geomagnetic storms and substorm activity on the radiation belts, as well as transient phenomena such as bursty bulk flows or dipolarization fronts. This FG additionally encompasses studies evaluating the magnetotail as a source of radiation belt particles, such as the evaluation of how often and in which conditions the plasma sheet acts as a source of energetic radiation belt particles, and the effect of these particle injections on inner magnetospheric wave generation and the subsequent wave-particle interactions.

The Earth’s inner magnetosphere is composed of a range of plasma population, such as the ring current and plasmasphere, that interact with the radiation belts. For example, different wave modes arise inside and outside the plasmasphere, so the plasmapause plays a key role in defining the spatial extent and key characteristics of inner magnetospheric waves that interact with radiation belt particles, while the ring current results in phenomena such as the Dst effect.

Determining the coupling of the atmosphere/ionosphere system on the radiation belt includes both the effects of the radiation belts on the atmosphere/ionosphere and the effects that the atmosphere/ionosphere have on the radiation belt environment. Radiation belt particle precipitation deposits mass and energy into the atmosphere/ionosphere, which can have significant space weather and climatological impacts. This FG therefore encompasses studies related to the pitch-angle scattering of radiation belt particles that results in precipitation, which can occur through a range of interactions (including non-linear interactions) with inner magnetospheric waves. Ionospheric outflow is also a source of inner magnetospheric particles, and multiple current systems couple the inner magnetosphere and ionosphere; evaluation of the impacts of these phenomena, and other ionospheric or atmospheric dynamics, on the radiation belts are in-scope for this FG.

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