质子带的变化可以追溯到风云1c卫星观测

IF 2.9 3区 地球科学
ChunQin Wang, Zheng Chang, XiaoXin Zhang, GuoHong Shen, ShenYi Zhang, YueQiang Sun, JiaWei Li, Tao Jing, HuanXin Zhang, Ying Sun, BinQuan Zhang
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引用次数: 1

摘要

本文利用风云1c卫星2000年3月25日至4月18日在近地轨道(~800 km)观测到的捕获质子的历史数据,选取5-10 MeV、10-40 MeV、40-100 MeV和~ 100-300 MeV的数据,分析质子的变化。在此期间,只有一次孤立的强风暴与太阳质子事件有关,并且没有受到先前质子变化的影响。这种扰动对质子捕获和损失的复杂动力学现象的影响随能量和L位置的不同而不同。5 ~ 10 MeV的质子通量增加并产生新的俘获,在L ~2.0处达到最大值,且峰值通量显著高于南大西洋异常中心。但在较高L时,通量损失明显,外边界从L ~2.7向L ~2.5后退。10-40 MeV质子通量的增加与5-10 MeV通量的增加相似;但峰值通量强度低于南大西洋异常中心。10-40 MeV质子通量的损失更接近地球一侧,外边界从L ~2.3减小到L ~2.25。对于40-100 MeV和100-300 MeV的高能质子,没有发现新的俘获现象。观察到40 ~ 100 MeV质子的损失,外边界从L ~2.0移到L ~1.9。100-400 MeV的质子损失不明显,分布在L <内;1.8. 在强磁暴的太阳质子注入区域,较低的能量更容易产生新的质子俘获,而在较宽的能量范围内发生损失,并使地球侧的外边界减小。NOAA-15卫星在同一时期观测到类似的动态变化,但FY-1C卫星在低能质子中观测到更复杂的变化。这些结果表明,不同l -壳层的质子的动力学行为是由俯仰角的不同引起的。还讨论了与新捕获和损失有关的可能机制。这些机制对于理解质子带在即将到来的太阳周期中的行为是非常重要的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Proton belt variations traced back to Fengyun-1C satellite observations

We used historical data to trace trapped protons observed by the Fengyun-1C (FY-1C) satellite at low Earth orbits (~800 km) and chose data at 5–10 MeV, 10–40 MeV, 40–100 MeV, and ~100–300 MeV from 25 March to 18 April 2000 to analyze the proton variations. Only one isolated strong storm was associated with a solar proton event during this period, and there was no influence from previous proton variations. Complex dynamic phenomena of proton trapping and loss were affected by this disturbance differently depending on the energy and L location. The flux of 5–10 MeV protons increased and created new trapping with a maximum at L ~2.0, and the peak flux was significantly higher than that at the center of the South Atlantic Anomaly. However, at higher L, the flux showed obvious loss, with retreat of the outer boundary from L ~2.7 to L ~2.5. The increase in the 10–40 MeV proton flux was similar to that of the 5–10 MeV flux; however, the peak flux intensity was lower than that at the center of the South Atlantic Anomaly. The loss of the 10–40 MeV proton flux was closer to the Earth side, and the outer boundary was reduced from L ~2.3 to L ~2.25. For the higher energy protons of 40–100 MeV and 100–300 MeV, no new trapping was found. Loss of the 40–100 MeV protons was observed, and the outer boundary shifted from L ~2.0 to L ~1.9. Loss was not obvious for the 100–400 MeV protons, which were distributed within L < 1.8. New proton trapping was more likely to be created at lower energy in the region of solar proton injection by the strong magnetic storm, whereas loss occurred in a wide energy range and reduced the outer boundary on the Earth side. Similar dynamic changes were observed by the NOAA-15 satellite in the same period, but the FY-1C satellite observed more complex changes in lower energy protons. These results revealed that the dynamic behavior of protons with different L-shells was due to differences in the pitch angle. Possible mechanisms related to new trapping and loss are also discussed. These mechanisms are very important for understanding the behavior of the proton belt in the coming solar cycle.

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来源期刊
Earth and Planetary Physics
Earth and Planetary Physics GEOSCIENCES, MULTIDISCIPLINARY-
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17.20%
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