Invading process of GCRs into the heliosphere S. Matsukiyo 1 , K. - - PowerPoint PPT Presentation

invading process of gcrs into the heliosphere
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Invading process of GCRs into the heliosphere S. Matsukiyo 1 , K. - - PowerPoint PPT Presentation

Invading process of GCRs into the heliosphere S. Matsukiyo 1 , K. Shimokawa 1 , H. Washimi 1,2 , T. Hada 1 1 Kyushu Univ., Japan 2 CSPAR, USA Background Solar modulation of CR spectrum Remarkable for E < a few 10 GeV Anisotropy for TeV


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Invading process of GCRs into the heliosphere

  • S. Matsukiyo1, K. Shimokawa1, H. Washimi1,2, T. Hada1

1Kyushu Univ., Japan 2CSPAR, USA

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SLIDE 2

Background

Solar modulation of CR spectrum  Remarkable for E < a few 10 GeV  Anisotropy for TeV CRs  Effect of convected spiral SW B field  Effect of large scale structures (TS, HP)  Effect of wave-particle interactions  Effect of non-stationarity of SW  …

Yuan [2018] NASA Abbasi et al. [2010]

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Background

Past approach  Diffusion-convection eq. based Yuan (2018), Aloisio et al. (2015), Yamazaki et al. (2015), …  Test particle simulation + global MHD simulation Lopez-Barquero et al. (2016, 2017), … ∆ = 20 AU 3500 AU

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Purpose

 To understand detailed process of GCR invasion into the heliosphere and further into the Earth  To reveal energy dependence of the invasion process Approach: Test particle simulation + high resolution global MHD simulation (∆ = 0.2 AU)

Washimi et al. [2015]

P T V B

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Test particle simulation + MHD simulation

provided by Washimi

Test particle simulation using , fields reproduced by MHD simulation

  • ,
  • # particles 10

No waves/turbulence Initial distribution function

  • - uniform on a sheet at a certain

in interstellar space

  • - monoenergetic jet along local field

10, 100 1000 ~ 10"#, 100 "# 1000"# $%&' 3)" #

%&' 23+,/.

/%&' 0.1/cc 1

%&' 63003

$&4 35)" #

&4 400+,/.

/

&4 5/

1

&4 1073

particles 8 9 : at 1AU

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Field lines

Z=0 Y=0 L1: draping $%&' connected to spiral $&4 L2: spiral $&4 L3: draping $%&' B/BISM

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Field structure

 Bow shock, heliopause, termination shock are reproduced.  The above discontinuities and SW current sheet form current layers. B J 9 :

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Particle behaviors (γ 10)

Y Z Z X X Y Z=0 Y=0 X=0  Most of particles follow L3 field lines and pass outside the HP or are mirror reflected at the HP  Some particles come in and out of the heliosphere when they come close enough to the heliopause along the draping IS B field lines  A part of them reach the inner boundary (r = 50AU) of the polar region  Very few particles reach the inner boundary after a short time (weeks)

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SLIDE 9

Particle behaviors (γ 10)

 Direction of field felt by a particle changes when it crosses the HP.  The particle stays near current sheet for a long time. < 0.013

Distance from the sun

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SLIDE 10

Particle behaviors (γ 1000)

 Direction of field felt by a particle changes when it crosses the HP.  They do not stay in the current sheet due to large gyro radii. < 1.3

Distance from the sun

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Particle behaviors (γ 1000)

 Easy to come in and out of the heliosphere due to large gyro radius  No mirror reflection for the particular case  Particles can reach the inner boundary (r = 50AU) with a short time  Some particles coil about the heliosphere even after that most of the

  • ther particles flow away.

Y Z Z X X Y Z=0 Y=0 X=0

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Statistics

Initial particle distribution: uniform on a 1/8 sphere velocity shell (uniform pitch angle) # particles reached at inner boundary

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Statistics

Energy dependence of anisotropy

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SLIDE 14

Summary

 Test particle simulation of CR invasion process using EB field obtained by global MHD simulation has been started.  Detailed analysis of particle behavior will be focused  Effect of wave-particle interaction will be incorporated  Statistics of particles will be discussed  …

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