scholarly journals Retrospective analysis of GLEs and estimates of radiation risks

2018 ◽  
Vol 8 ◽  
pp. A52 ◽  
Author(s):  
Leonty I. Miroshnichenko

28 February 2017 marked 75 years since the first confident registration of solar cosmic rays (SCRs), i.e., accelerated solar particles with energies from about 106 to ~1010 ÷ 1011 eV. Modern state of the problems related to the studies of Ground Level Enhancements (GLEs) of relativistic SCRs is critically analyzed based on available direct and proxy data. We are also taking into account extremely large fluxes of non-relativistic solar energetic particles (SEPs). Both kinds of SCR events are of great astrophysical and geo-scientific (geophysical) interests. A number of the GLE properties (total statistics, occurrence rate, longitude distribution, ranking of GLEs, a number of specific GLEs – so-called “rogue” SEP events etc.) are discussed in some detail. We note also the problems of GLE identification (definition) by ground-based observations, the difficulties in the studies of weak (“hidden”, or sub-) GLEs etc. One of serious challenges to the problem of radiation hazard in space is a lack of a clear, unambiguous relation between the fluxes (fluences) of relativistic SCR and non-relativistic SEPs. Special attention is paid to the recent debate on the validity, origin and properties of the “ancient” events AD775, AD994, AD1859 (Carrington event) and BC3372. We demonstrate that, in spite of existing uncertainties in proton fluences above 30 MeV, all of them are fitted well by a unique distribution function, at least, with the present level of solar activity. Extremely large SEP events are shown to obey a probabilistic distribution on their fluences with a sharp break in the range of large fluences (or low probabilities). The studies of this kind may be extended for periods with different levels of solar activity in the past and/or in the future. Dose rates at aircraft altitudes are also demonstrated during some GLEs. Several examples of using the SCR data and GLE properties in radiation prediction schemes are considered.

2011 ◽  
Vol 7 (4) ◽  
pp. 439-443 ◽  
Author(s):  
M. Andriopoulou ◽  
H. Mavromichalaki ◽  
P. Preka-Papadema ◽  
C. Plainaki ◽  
A. Belov ◽  
...  

2010 ◽  
Vol 50 (1) ◽  
pp. 21-33 ◽  
Author(s):  
A. V. Belov ◽  
E. A. Eroshenko ◽  
O. N. Kryakunova ◽  
V. G. Kurt ◽  
V. G. Yanke

2015 ◽  
Vol 79 (5) ◽  
pp. 561-565 ◽  
Author(s):  
A. V. Belov ◽  
E. A. Eroshenko ◽  
O. N. Kryakunova ◽  
N. F. Nikolayevskiy ◽  
A. M. Malimbayev ◽  
...  

Solar Physics ◽  
2010 ◽  
Vol 269 (1) ◽  
pp. 155-168 ◽  
Author(s):  
M. Andriopoulou ◽  
H. Mavromichalaki ◽  
C. Plainaki ◽  
A. Belov ◽  
E. Eroshenko

Author(s):  
Dung Nguyen Thanh ◽  
Minh Le Huy ◽  
Christine Amory-Mazaudier ◽  
Rolland Fleury ◽  
Susumu Saito ◽  
...  

This paper presents the variations of the rate of change of Total Electron Content (TEC) index (ROTI), characterizing the occurrence of ionospheric plasma irregularities over Vietnam and neighboring countries in the Southeast Asian region using the continuous GPS data during the 2008-2018 period. The results showed that the occurrence of strong ROTI in all stations is maximum in equinox months March/April and September/October and depends on solar activity. The ROTI is weak during periods of low solar activity and strong during periods of high solar activity. There is an asymmetry between the two equinoxes. During maximum and declining phases of 2014-2016, occurrence rates in March equinox are larger than in September equinox, but during the descending period of 2010-2011, the occurrence rates in September equinox at almost all stations are larger than in March equinox. The correlation coefficients between the monthly occurrence rate of irregularities and the F10.7 solar index at the stations in the equatorward EIA crest region are higher than at those in the magnetic equatorial and the poleward EIA crest regions. The irregularity occurrence is high in the pre-midnight sector, maximum between 2000 LT to 2200 LT. The maximum irregularity occurrence is located around 4-5° degrees in latitude equator-ward away from the anomaly crests.


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