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Space Physics and Aeronomy, Space Weather Effects and Applications


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another type of space radiation impact within the Earth environment is shown in Figure 1.4c. This is called surface charging. If the space system is subject to hot plasma in its environment and photo‐electrons are not able to carry away charge promptly from insulator and dielectric material (as happens in solar eclipse conditions or on the nonilluminated side of a space vehicle), there can be a strong buildup of charge on key areas of the spacecraft surface. When the charge buildup is sufficient, a sudden discharge can result. This may produce material damage and/or a significant electromagnetic discharge around the spacecraft. Such effects cause phantom electromagnetic signals or changes of state in memory systems. There can even be permanent damage to electronics (see Bodeau and Baker, chapter 2, this volume).

Schematic illustration of a modern-day view of the Earth’s radiation belts as observed by the Van Allen Probes mission.

      (Source: Baker, 2005. Reproduced with permission from Springer Nature.)

Schematic illustration of a modern-day view of the Earth’s radiation belts as observed by the Van Allen Probes mission.

      (Source: Marvin & Gorney, 1991); reprinted by permission of the American Institute of Aeronautics and Astronautics, Inc.

      Solar energetic particle events are the mechanism by which very high‐energy protons appear in the outer zone region of the radiation belts. However, these events are very short lived (hours in duration), as the high‐energy protons with such large gyro‐radii are not able to be stably trapped at these locations. As noted, they can often penetrate to the inner zone, where stronger magnetic fields in a more rigid magnetic topology can entrain these particles for long times. In general, highly energetic protons (multi‐MeV energies) are not considered to be a regular feature in the outer zone (see Selesnick et al., 2014).

Schematic illustration of a modern-day view of the Earth’s radiation belts as observed by the Van Allen Probes mission.

      (Source: X. Li.)

      As is evident from the figure, the outer Van Allen belt (as monitored from the ~500 km altitude of SAMPEX) typically extends from L ~ 3.0 to roughly L = 6.5. However, the belt’s spatial extent was highly variable over the ~20‐year SAMPEX lifetime. Also, the peak electron flux levels varied widely as a function of time. For example, in 1994, the peak >2 MeV electron fluxes were over 104 electrons/cm2‐s‐sr, while in 2008–2009 the electron flux was often barely above background levels (~100 electrons/cm2‐s‐sr). As is obvious from inspection of the figure, a main controller of the electron fluxes in the outer belt is the solar wind speed impacting Earth’s magnetosphere (Baker et al., 1987). Indeed, solar wind speeds with V > 500 km/sec generally are associated with high outer radiation belt electron “content” (Baker, 2004). On the other hand, persistent solar wind speeds of V ≤ 300 km/sec can lead to virtual disappearance of the outer belt (for electron energies E ≳1MeV). This occurred quite prominently in the profound solar minimum of 2008–2009.

      The inner “edge” of the outer zone, as is obvious in Figure 1.6, shows considerable variability in spatial location. During particularly strong solar wind forcing conditions, the inward extent of the outer zone population can appear to reach down to L ~ 2.5. This is typically a rare and brief circumstance. During truly extreme forcing events such as the Halloween Storm events of late 2003 (see Baker et al., 2004), the slot region can be filled with multi‐MeV electrons for weeks of time. An event of great strength was also seen in late 2004 (see Figure 1.6).