Trapped antiprotons in the Earth inner radiation belt in PAMELA experiment

2011 ◽  
Vol 75 (6) ◽  
pp. 854-856
Author(s):  
Yu. T. Yurkin ◽  
O. Adriani ◽  
G. Barbarino ◽  
G. A. Bazilevskaya ◽  
R. Bellotti ◽  
...  
AIAA Journal ◽  
1963 ◽  
Vol 1 (2) ◽  
pp. 516-519
Author(s):  
S. N. VERNOV ◽  
I. A. SAVENKO ◽  
P. I. SHAVRIN ◽  
V. I. NESTEROV ◽  
N. F. PISARENKO

2021 ◽  
Vol 3 ◽  
pp. 47-57
Author(s):  
I. N. Myagkova ◽  
◽  
V. R. Shirokii ◽  
Yu. S. Shugai ◽  
O. G. Barinov ◽  
...  

The ways are studied to improve the quality of prediction of the time series of hourly mean fluxes and daily total fluxes (fluences) of relativistic electrons in the outer radiation belt of the Earth 1 to 24 hours ahead and 1 to 4 days ahead, respectively. The prediction uses an approximation approach based on various machine learning methods, namely, artificial neural networks (ANNs), decision tree (random forest), and gradient boosting. A comparison of the skill scores of short-range forecasts with the lead time of 1 to 24 hours showed that the best results were demonstrated by ANNs. For medium-range forecasting, the accuracy of prediction of the fluences of relativistic electrons in the Earth’s outer radiation belt three to four days ahead increases significantly when the predicted values of the solar wind velocity near the Earth obtained from the UV images of the Sun of the AIA (Atmospheric Imaging Assembly) instrument of the SDO (Solar Dynamics Observatory) are included to the list of the input parameters.


2020 ◽  
Author(s):  
Eldho Midhun Babu ◽  
Hilde Nesse Tyssøy ◽  
Christine Smith-Johnsen ◽  
Ville Aleksi Maliniemi ◽  
Josephine Alessandra Salice ◽  
...  

<p>Energetic electron precipitation (EEP) from the plasma sheet and the radiation belts, can collide with gases in the atmosphere and deposit their energy. EEP increase the production of NOx and HOx, which will catalytically destroy stratospheric ozone, an important element of atmospheric dynamics. The particle precipitation also causes variation in the radiation belt population. Therefore, measurement of latitudinal extend of the precipitation boundaries is important in quantifying atmospheric effects of Sun-Earth interaction and threats to spacecrafts and astronauts in the Earth’s radiation belt. <br>This study uses measurements by MEPED detectors of six NOAA/POES and EUMETSAT/METOP satellites during the year 2010 to determine the latitudinal boundaries of EEP and its variability with geomagnetic activity and solar wind drivers. Variation of the boundaries with respect to different particle energies and magnetic local time is studied. The result will be a key element for constructing a model of EEP variability to be applied in atmosphere climate models.</p>


AIAA Journal ◽  
1963 ◽  
Vol 1 (2) ◽  
pp. 520-521
Author(s):  
E. V. GORCHAKOV

2019 ◽  
Vol 46 (11) ◽  
pp. 348-350
Author(s):  
T. R. Zharaspayev ◽  
S. V. Koldashov ◽  
V. V. Mikhailov

Author(s):  
S. N. Kuznetsov ◽  
I. N. Myagkova ◽  
E. A. Muravieva ◽  
B. Yu. Yushkov ◽  
L. I. Starostin ◽  
...  

2021 ◽  
Author(s):  
Frances Staples ◽  
Jonathan Rae ◽  
Adam Kellerman ◽  
Kyle Murphy ◽  
Jasmine Sandhu ◽  
...  

<p>Loss mechanisms act independently or in unison to drive rapid loss of electrons in the radiation belts. Electrons may be lost by precipitation into the Earth’s atmosphere, or through the magnetopause into interplanetary space. Whilst this magnetopause shadowing is well understood to produce dropouts in electron flux, it is less clear if shadowing continues to remove particles in tandem with electron acceleration processes, limiting the overall flux increase. </p><p>We investigate the contribution of shadowing to overall radiation belt fluxes throughout a geomagnetic storm in early September 2017. We use new, multi-spacecraft phase space density calculations to decipher electron dynamics during each storm phase and identify features of magnetopause shadowing during both the net-loss and the net-acceleration storm phases. We also highlight two distinct types of shadowing; ‘Indirect’, where electrons are lost through ULF wave driven radial transport towards the magnetopause boundary, and ‘direct’, where electrons are lost as their orbit intersects the magnetopause. </p>


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