scholarly journals Simulation study of the energetic neutral atom (ENA) imaging monitoring of the geomagnetosphere on a lunar base

2021 ◽  
Vol 7 (3) ◽  
pp. 3-11
Author(s):  
Lu Li ◽  
Yu Qing-Long ◽  
Zhou Ping ◽  
Zhang Xin ◽  
Zhang Xian-Guo ◽  
...  

Since the moon’s revolution cycle is exactly the same as its rotation cycle, we can only see the moon always facing Earth in the same direction. Based on the clean particle radiation environment of the moon, a neutral atomic telemetry base station could be established on the lunar surface facing Earth to realize long-term continuous geomagnetic activity monitoring. Using the 20°×20° field of view, the 0.5°×0.5° angle resolution, and the ~0.17 cm²sr geometric factor, a two-dimensional ENA imager is being designed. The magnetospheric ring current simulation at a 4–20 keV energy channel for a medium geomagnetic storm (Kp=5) shows the following: 1) at ~60 Rᴇ (Rᴇ is the Earth radius), the imager can collect 10⁴ ENA events for 3 min to meet the statistical requirements for 2D coded imaging data inversion, so as to meet requirements for the analysis of the substorm ring current evolution process of magnetic storms above medium; 2) the ENA radiation loss puzzles in the magnetopause and magnetotail plasma sheet regions have been deduced and revealed using the 2-D ENA emission model. High spatial-temporal resolution ENA imaging monitoring of these two important regions will provide the measurement basis for the solar wind energy input process and generation mechanism; 3) the average sampling interval of ENA particle events is about 16 ms at the moon’s orbit; the spectral time difference for the set energy range is on the order of minutes, which can provide location information to track the trigger of geomagnetic storm particle events.

2021 ◽  
pp. 3-10
Author(s):  
Lu Li ◽  
Yu Qing-Long ◽  
Zhou Ping ◽  
Zhang Xin ◽  
Zhang Xian-Guo ◽  
...  

Since the moon’s revolution cycle is exactly the same as its rotation cycle, we can only see the moon always facing Earth in the same direction. Based on the clean particle radiation environment of the moon, a neutral atomic telemetry base station could be established on the lunar surface facing Earth to realize long-term continuous geomagnetic activity monitoring. Using the 20°×20° field of view, the 0.5°×0.5° angle resolution, and the ~0.17 cm²sr geometric factor, a two-dimensional ENA imager is being designed. The magnetospheric ring current simulation at a 4–20 keV energy channel for a medium geomagnetic storm (Kp=5) shows the following: 1) at ~60 Rᴇ (Rᴇ is the Earth radius), the imager can collect 10⁴ ENA events for 3 min to meet the statistical requirements for 2D coded imaging data inversion, so as to meet requirements for the analysis of the substorm ring current evolution process of magnetic storms above medium; 2) the ENA radiation loss puzzles in the magnetopause and magnetotail plasma sheet regions have been deduced and revealed using the 2-D ENA emission model. High spatial-temporal resolution ENA imaging monitoring of these two important regions will provide the measurement basis for the solar wind energy input process and generation mechanism; 3) the average sampling interval of ENA particle events is about 16 ms at the moon’s orbit; the spectral time difference for the set energy range is on the order of minutes, which can provide location information to track the trigger of geomagnetic storm particle events.


2016 ◽  
Vol 34 (1) ◽  
pp. 75-84 ◽  
Author(s):  
V. Pierrard ◽  
G. Lopez Rosson

Abstract. With the energetic particle telescope (EPT) performing with direct electron and proton discrimination on board the ESA satellite PROBA-V, we analyze the high-resolution measurements of the charged particle radiation environment at an altitude of 820 km for the year 2015. On 17 March 2015, a big geomagnetic storm event injected unusual fluxes up to low radial distances in the radiation belts. EPT electron measurements show a deep dropout at L > 4 starting during the main phase of the storm, associated to the penetration of high energy fluxes at L < 2 completely filling the slot region. After 10 days, the formation of a new slot around L = 2.8 for electrons of 500–600 keV separates the outer belt from the belt extending at other longitudes than the South Atlantic Anomaly. Two other major events appeared in January and June 2015, again with injections of electrons in the inner belt, contrary to what was observed in 2013 and 2014. These observations open many perspectives to better understand the source and loss mechanisms, and particularly concerning the formation of three belts.


2007 ◽  
Vol 40 (3) ◽  
pp. 338-341 ◽  
Author(s):  
J.H. Adams ◽  
M. Bhattacharya ◽  
Z.W. Lin ◽  
G. Pendleton ◽  
J.W. Watts

1993 ◽  
Vol 98 (E9) ◽  
pp. 17127 ◽  
Author(s):  
C. M. Pieters ◽  
J. W. Head ◽  
J. M. Sunshine ◽  
E. M. Fischer ◽  
S. L. Murchie ◽  
...  
Keyword(s):  
The Moon ◽  

2017 ◽  
Vol 212 (3-4) ◽  
pp. 1069-1106 ◽  
Author(s):  
Nathan A. Schwadron ◽  
John F. Cooper ◽  
Mihir Desai ◽  
Cooper Downs ◽  
Matt Gorby ◽  
...  

Space Weather ◽  
2014 ◽  
Vol 12 (6) ◽  
pp. 329-336 ◽  
Author(s):  
Jamie A. Porter ◽  
Lawrence W. Townsend ◽  
Harlan Spence ◽  
Michael Golightly ◽  
Nathan Schwadron ◽  
...  

2021 ◽  
Vol 44 ◽  
pp. 7-11
Author(s):  
Elena Antonova ◽  

We analyzed the problems of formation of the outer radiation belt (ORB) taking into consideration the latest changes in our understanding of the high-latitude magnetospheric topology. This includes strong evidence that the auroral oval maps to the outer part of the ring current, meanwhile the ORB polar boundary maps inside the auroral oval. Our analysis also includes the variation of the plasma pressure distribution and the time of the acceleration of relativistic electrons during geomagnetic storm. It is shown that the maximum of ORB is formed after the geomagnetic storm in the region of plasma pressure maximum. The position of this maximum agrees with the prediction of the ORB formation theory based on the analysis of ring current development during storm. We emphasize the role of adiabatic processes in the ORB dynamics and the importance of the substorm injections during storm recovery phase for the formation of enhanced fluxes of ORB electrons after the storm.


Author(s):  
GIOVANNI DE ANGELIS ◽  
FRANCIS F. BADAVI ◽  
JOHN M. CLEM ◽  
STEVE R. BLATTNIG ◽  
MARTHA S. CLOWDSLEY ◽  
...  

2009 ◽  
Vol 147 (3-4) ◽  
pp. 187-231 ◽  
Author(s):  
Rami Vainio ◽  
Laurent Desorgher ◽  
Daniel Heynderickx ◽  
Marisa Storini ◽  
Erwin Flückiger ◽  
...  

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