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Inner Magnetosphere`s effects on Radiation Belt

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    ruc ure an ynam cs o nner

    MagnetosphereMagnetosphere

    and Their Eects on Radiation Beltand Their Eects on Radiation Belt

    ElectronsElectrons

    Chia-Lin uang Boston University, MA, USA

    CISM Seminar, March 24th, 2008

    Special thanks: Harlan Spence, Mary H!son, "ohn #yon, "e$ H%hes, Ho&ar! Sin%er, Scot 'lkin%ton, an! many more

     APL

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    (oals o) my *esearch(oals o) my *esearch

     +o n!erstan! the physics !escriin% the strctre an!!ynamics o) -el! con-%rations in the inner

    ma%netosphere

     +o assess the per)ormance o) %loal ma%netospheric

    mo!els n!er varios con!itions

     +o .anti)y the response o) %loal ma%netic an! electric

    -el!s to solar &in! variations, an! ltimately their e$ects

    on ra!ial transport o) ra!iation elt electrons/

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    Motivation: *a!iation BeltsMotivation: *a!iation Belts

    iscovery o) 1an Allen ra!iationelts '3plorer , 568

     +rappe! protons 7 electrons,

    spatial !istrition 29 *';,

    ener%y

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    ynamical *a!iation Beltynamical *a!iation Belt

    'lectrons'lectrons

    =hy st!y ra!iation

    elt electrons>

    Becase they are

    physically interestin%

    *a!iation !ama%e to

    spacecra)t an! hman

    activity in space

    (oal: !escrie an!pre!ict ho& ra!iation

    elts evolves in time at

    a %iven point in spaceGreen [2002]

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    Solar =in! an! Ma%netosphereSolar =in! an! Ma%netosphere

    Avera%e pictre o) solar &in! an! ma%netosphere ma%netic -el!,

    re%ions, inner ma%/ plasmas;

    1ariations o) ?s&, IM@ B cases ma%netospheric !ynamics

    Ring Current

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    Ma%netic StormsMa%netic Storms Most intense solar

    &in!9ma%netospherecoplin%

    IM@ B soth&ar!,

    stron% electric -el! in

    the tail

    @ormation o) rin%

    crrent an! its e$ect to-el! con-%rations

    st measres rin% crrent !evelopment

    Storm s!!en commencement SSC;,main phase, an! recovery phase

    ration: !ays

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    Ma%netospheric ?lsationsMa%netospheric ?lsations

    Ultra9lo&9)re.ency U#@; MH &aves @re.ency an! time scale: 29 mH, 90 mintes

    @iel! ctation ma%nit!e

    @irst oserve! in 5th centry

    =aves stan!in% alon% the ma%netic -el! lines connect toionospheres Dungey , 564D

    Morpholo%y an! %eneration mechanisms are not )lly

    n!erstoo!

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    (loal Ma%netospheric Mo!els(loal Ma%netospheric Mo!els ?rovi!e %loal B an! ' -el!s nee!e! )or ra!iation elt st!y

    ata9ase!: +sy%anenko mo!els ?arameterie!, .ansi9static state o) avera%e ma%netic -el!

    con-%rations

    ?hysics9ase!: (loal MH co!e

    Sel)9consistent, time !epen!ent, realistic ma%netosphere

    Importance an! applications, vali!ation o) the %loal mo!els

       '  m  p   i  r   i  c

      a   l  m  o   !  e   l

       (   l  o   ,  a   l   M   H   0  s   i  m     l  a   t   i  o  n

    #@M MH co!e +sy%anenko mo!el

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    Char%e! ?article Motion inChar%e! ?article Motion in

    Ma%netosphereMa%netosphere (yro, once an! !ri)t motions

    (yro

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    =hy is it so Har!> =hat =ol!=hy is it so Har!> =hat =ol!

    Help>Help>

    ?ropose! physical processes !cceleration: lar%e9 an! small9scale recirclations, heatin% y

    =histler &aves, ra!ial !i$sion y U#@ &aves, csp sorce,sstorm inEection, s!!en implse o) solar &in! pressre an!etc/

    Loss: pitch an%le !i$sion, Colom collision, an!Ma%netopase sha!o&in%/

    Transport

    iFclties to !i$erentiate the mechanisms:

    #ack o) Measrements #ack o) an accrate ma%netic an! electric -el! mo!el

    Convertin% particle 3 to !istrition )nction is tricky

    Gee! etter n!erstan!in% o) &ave9particle interactions

    Comptational resorce

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     +he *est o) the +alk +he *est o) the +alk

    Ma%netospheric -el! !ynamics: !ata 7 mo!els #ar%e9scale: Ma%netic storms

    Small9scale: U#@ &ave -el!s

    '$ects o) -el! !ynamics on ra!iation eltelectrons

    Create &ave -el! simlations

    anti)y electron ra!ial transport in the &ave -el!s

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    #yon9@e!!er9Moary Co!e#yon9@e!!er9Moary Co!e #yon et al/2004D

    Uses the i!eal MH e.ations to mo!el the interactionet&een the solar &in!, ma%netosphere, an! ionosphere

    Simlation !omain an! %ri!

    2 electrostatic ionosphere

    Solar &in! inpts

    @iel! con-%rations an!

    &ave -el! vali!ations y

    comparin% & (J'S !ata

    LFM grid in equatorial plane

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    ataMo!el Case St!yataMo!el Case St!y

    2492K Septemer 558 maEor storm event st minimm 92L n+;

    #@M inpts: solar &in! an! IM@ !ata

    (eosynchronos orit

    Sep98 event: solar wind data and Dst

    Compare #@M an! (J'S B9-el!at ('J orit

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    Statistical ataMo!elStatistical ataMo!el

    ComparisonsComparisons

    5 ma%netic storms 29month non9storm

    interval

    #@M -el! lines are

    consistently n!er9

    stretche!, especially!rin% storm9time, on

    the ni%htsi!e

    ?re!ict reasonale

    non9storm time -el!

    Improvements o) #@M

    Increase %ri!

    resoltion

    A!! rin% crrent

    Field residual B = BMHD – B!"S

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    a s ca compar son o +sy%anenko mo!els an! (J'S +sy%anenko mo!els an! (J'S

    !ata!ata 62 maEor ma%netic storm )rom 55K to 2004

     +S06 has the est per)ormance in all local time an! storm levels

    #nder$esti%ate

    &er'e(t predi(tion

    !ver$esti%ate

    Field residual B = B!"S – B)%odel

    )9* )+, )S+-

    ) - l! ! lC ) - l! ! l

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    Conse.ence o) -el! mo!elConse.ence o) -el! mo!el

    errorserrors Inaccrate B9-el! mo!el col! alter the reslts o) relate! st!ies

    '3ample: ra!ial pro-les o) phase space !ensity o) ra!iation elt electrons

    iscrepancies et&een +sy%anenko mo!els sin% same inpts

    Mo!el -el! lines trace! )rom (J'S98Ns position le)t;

    ?itch an%les at (J'S98Ns position an! at ma%netic e.ator ri%ht;

    ~15% errorbetween T96

    and TS05

    U#@ =

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    U#@ =aves naves nMa%netosphereMa%netosphere

    =ave sorces: shear o&, variation in the solar &in! pressre, IM@ B, an!instaility etc/

    ?revios st!ies: inte%rate! &ave po&er, &ave occrrence

    Ge3t, calclate &ave po&er as )nction o) )re.ency sin% (J'S !ata

    &ave -el! pre!iction o) #@M an! + mo!el/

    NASA

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    ?o&er Spectral ensity ?S;?o&er Spectral ensity ?S;

    Calclate ?S sin% L9

    hor (J'S B9-el! !ata

    ?roce!res:

    /  +ake ot s!!en -el!

    chan%e

    2/ e9tren! &

    polynomial -t

    L/ e9spike & L stan!ar!

    !eviations

    4/ Hi%h pass -lter 0/6mH;

    6/ @@+ to otain ?S

    n+2HD

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    (J'S B9-el! ?Ss in @AC(J'S B9-el! ?Ss in @AC

    5 years o) (J'S !ata (98, (95 an! (90satellites;

    @iel!9ali%ne! coor!inates

    Separate into L9hor intervals 8 local time sectors;

    Calclate ?Ss

    Me!ian ?S in each )re.ency in

    "oon

    Midnight

    Da#nDus$ 

    Co%pressional ./i%ut0al Radial

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    Sortin% (J'S BSortin% (J'S B ?S y S= 13?S y S= 13

       ?   S   0

       B   C  n   +   2   I   H  A   D

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    Sortin% (J'S BSortin% (J'S B ?S y IM@ B?S y IM@ B

       ?   S   0

       B   C  n   +   2   I   H  A   D

         !  "  o  #   t   $  w

      a  r   d

         !  n  o  r   t   $  w  a  r   d

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    U#@ =aves in #@M co!eU#@ =aves in #@M co!eirect comparisons o) U#@ &aves !rin% @e9Apr 55K in -el!9

    ali%ne! coor!/

       ?   S   0

       B   C  n   +   2   I   H  A   D

    Lo(al )i%e

       L   F   M   o  u

       t  p  u   t

       

       !   "   S   d  a   t  a

    B1 o&'re""(ona)

    Bn 

    rad(a)

    B2

    a!(t$a)

    *#$

    better t$ane+'eted,

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    st an! Op e$ects on U#@ &avest an! Op e$ects on U#@ &ave

    po&erpo&er

    Hig0 3p interval

    -' . 4

    Low 3p interval-' / 4

    Hig0 Dst interval Low Dst interval

      "t 40 nT "t 40 nT

    U#@ &ave po&er

    has hi%her

    !epen!ence on Op

    than st

    'ven tho%h #@M

    !oes not

    repro!ce per)ect

    rin% crrent, it

    pre!ictsreasonale -el!

    pertrations

    U#@ &ave pre!iction o) +sy%anenkoU#@ &ave pre!iction o) +sy%anenko

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    U#@ &ave pre!iction o) +sy%anenkoU#@ &ave pre!iction o) +sy%anenko

    mo!elmo!el

       )   S   +   -  %  o   d  e   l

       L   F   M   (  o   d  e

          !   "   S   d  a   t  a

    Un!erestimates

    the &ave po&er

    at

    %eosynchronos

    orit

    @iel! ctations

    are reslts o) an

    e3ternal !river

    #ack o) the

    internal physical

    processes

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    Smmary o) Mo!elSmmary o) Mo!el

    ?er)ormance?er)ormance

    Use #@MNs &ave -el!s !rin% non9storm time to st!y U#@

    &ave e$ects on ra!iation elt electrons

    Sch con!itions e3ist !rin% hi%h spee! solar &in!

    streams intervals/

    U#@ = '$ t *BU#@ =ave '$ects on *B

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    U#@ =ave '$ects on *BU#@ =ave '$ects on *B

    'lectrons'lectrons Stron% correlation et&een U#@ &ave po&er an! ra!iation

    elt electron 3 Rostoker et al., 558D

    ri)t resonant theory Hudson et al., 555 an! Elkington et al., 555D

    U#@ &aves can e$ectively accelerate relativistic electrons

    antitative !escription o) &ave9particle interaction

    o"toer et a) [1998]

    )(nton et a) [2003]

    ? i l i$ i i? ti l i$ i i

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    ?article i$sion in?article i$sion in

    Ma%netosphereMa%netosphere

    Diusion theory% timeevoltion o) a !istrition

    o) particles &hose

    traEectories are !istre!

    y innmerale small,

    ran!om chan%es/

    ?itch an%le !i$sion loss;:

    violate st or 2n! invariant

    *a!ial !i$sion transport

    an! acceleration;: violate

    Lr! invariant

    ( )

    ∂=

    ∂ f   L

     L L D

     Lt 

     f   LL

    2

    2

    1[ ]1

    2

    2

    −∆

    =   day L

     D LLτ 

    ad(a) d(::#"(on oe::((ent;ad(a) d(::#"(on e

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    *a!ial i$sion CoeFcient,*a!ial i$sion CoeFcient,

    ####

    #ar%e !eviations in previosst!ies

    ?ossile shortcomin%s

    Jver simpli-e! theoretical

    assmptions

    #ack o) accrate ma%netic -el!

    mo!el an! &ave -el! map

    InsFcient measrement

    M/ =altNs s%%estion: )ollo& *B

    particles in realistic

    ma%netospheric con-%rations

    =alt 554D

    E&perimental 'solid( and

    theoretical 'dashed( DLL )alues

    =hen oes #@M ?re!ict =aves=hen oes #@M ?re!ict =aves

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    =hen oes #@M ?re!ict =aves=hen oes #@M ?re!ict =aves

    =ell>=ell>

    (J'S an! #@M ?Sssorte! y solar &in!

    13 ins

    #@M !oes etter !rin%

    mo!erate activities

    Create U#@ &ave

    activities y !rivin%

    the #@M co!e &ith

    synthetic solar &in!

    pressre inpt

    4 !

    ! !

    o ar = n ?ressreo ar n ressre

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    o ar = n ?ressreo ar n ressre1ariation1ariation

    Histo%rams o) solar &in! !ynamic

    pressre )rom 5 years o) =in! !ata )or13 P *++, ,++, an! ++ kms ins

    Make time9series pressre variations

    proportional to solar &in! 13

    Synthetic Solar =in! ?ressreSynthetic Solar =in! ?ressre

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    Synthetic Solar =in! ?ressreSynthetic Solar =in! ?ressre13;13;

    #@M inpts: Constant 13 variation in nmer !ensity/

    Gorth&ar! IM@ B Q2 n+;, to isolate pressre !riven &aves/

    I!ealie! #@M 13 simlations sin% hi%h time an! spatial resoltions

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    I!ealie! 13 SimlationsI!ealie! 13 Simlations

    (J'S statisticalst!y 5 years!ata; as )nctiono) 13 Rmostlynorth&ar! IM@;

    rive #@M topro!ce Rreal U#@&aves &ith solar&in! !ynamicpressre variationsas )nction o) 13Rprelynorth&ar! IM@;   #

       @   M

       1  3

      r    n  s

       (   J   '   S   !  a   t  a

    .& / *++ .& / ,++ .&/++

    ' = ? S ti l' =a e ?o er Spatial

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    'T =ave ?o&er Spatial'T =ave ?o&er Spatial

    istritionsistritions

    =ave po&er increases as 13 ?! variations; increases

    =ave amplit!e is hi%her at lar%er ra!ial !istance &ave sorce;

    ])/[()(   2

    6

    5.0

    mmV df   f   PSD power Wave

    mHz 

    mHz 

     E 

    ∫ =

    ϕ 

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    *a!iation Belt Simlations*a!iation Belt Simlations

    Test particle code 'lkin%ton et al/, 2004D

    Satis)y st a!iaatic invariant (i!in% center appro3imation

    50o pitch an%le electron

    ?sh particles sin% #@M ma%netic an! electric-el!s

    Simlate particles in

    #@M 13 P 400 an! K00 kms rns

    ?article initial con!itions

    @i3e! P 800 Me1(

    *a!ial: 4 to 8 *'

    o aimthal !irection

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    *ate o) 'lectron *a!ial +ransport*ate o) 'lectron *a!ial +ransport####;;

    Convert particle location to #V Roederer , 50D

    Calclate or ra!ial !i$sion coeFcient, ##13; τ 2

    2 L D LL

    ∆=

    DLL in(reases wit0 L

    DLL 

    in(reases

    wit0 56

    Φ

    −=

     E  R

    k  L

      0*  2π 

    CC l1 l I

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    Compare Compare #### 1ales I1ales I

     +he maEor !i$erences

    et&een previosst!ies an! this &ork

    Amplit!e o) &ave -el!

    IM@ B

    Ma%netic -el! mo!el

    ?article ener%y Calclatin% metho!

     +heoretical assmption

    i$erences make it

    impossile )or a )air

    comparison

    Hi%hli%ht: Selesnick et al. 55D

    ∆ ~10 nT

    ∆ ~1 nT

    ∆ ~2 nT

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    Compare Compare #### 1ales II1ales II

    ## < !B

    2

     Schulz and Lanzerotti, 54D

    A)ter scalin% )or &ave po&er

    Compare to Selesnick et al. 

    55D a%ain

    Match &ell &ith 13PK00 kms

    interval #9!epen!ent;

    Avera%e 13 o) Selesnick et al. 

    200D an! IM@ B e$ect

     +his s%%ests that ra!ial

    !i$sion is &ell9simlate!, can

    !i$erentiate )rom other physical

    processes

    ##13, B, ∆?!yn, Op etc/;

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    SmmarySmmary

     +S06 est pre!icts ('J ma%netic -el!s in all con!itions

    #@M has %oo! pre!ictions o) .iet time -el!s, t not )orstorm time

    U#@ &ave strctres an! amplit!es at ('J sorte! yselecte! parameters

    U#@ &ave -el! pre!ictions: #@M is very %oo!, t not +S06

    *a!ial !i$sion coeFcient !erive! )rom MH?article co!e

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    Conclsions an! AchievementsConclsions an! Achievements

    Most comprehensive, in!epen!ent st!y o) state9o)9the9artempirical ma%netic -el! mo!els

    Most .antitative investi%ation o) %loal MH simlations inthe inner ma%netosphere

    Most comprehensive oservational U#@ &ave -el!s at%eosynchronos orit !e!icate! to oter one electronst!y

    @irst e3ploration on U#@ &ave -el! per)ormance o) %loalma%netospheric mo!els

    @irst ## calclation y )ollo&in% relativistic electrons in

    realistic, sel)9consistent -el! con-%rations an! &ave -el!so) an MH co!e