5
A TOOL TO MODEL SOLAR ENERGETIC PARTICLE EVENTS.
1 2;3 1
D. Lario , B. Sanahuja , A.M. Heras
1
Space Science Department, ESTEC/ESA, 2200AG No ordwijk, The Netherlands
2
Dept. Astronomia i Meteorologia, Universitat de Barcelona, Barcelona, Spain
3
Institut d'Estudis Espacials de Catalunya, Barcelona, Spain
ABSTRACT may also expand through the heliosphere driving a
sho ckwave across the interplanetary medium. The
b ehavior of the sho cks close to the Sun and through
interplanetary space is quite di erent Cane, 1997.
Gradual solar energetic particle events p ose a serious
While strong sho cks may extend up to 300 in longi-
risk to spacecraft comp onents. The origin of these
tude near the corona, they extend at most 180 at 1
particle events is closely asso ciated with the devel-
AU Cliver et al., 1995.
opment of coronal mass ejections and sho ck waves
driven by them. Prediction of uences observed at
As the sho ckgoesaway from the Sun, it crosses many
di erent heliospheric p ositions during these events re-
IMF lines and may be resp onsible for accelerating
quires to know the physical pro cesses o ccurring dur-
particles to energies much higher than the thermal
ing their development. We outline the main ingre-
solar wind background Sanahuja & Domingo [1987]
dients of a mo del that repro duces particle ux and
and references therein. These energetic particles
anisotropy pro les of these events. This mo del in-
propagate along the IMF lines owing outward from
cludes a simulation of the propagation of the asso ci-
the sho ck and arriving at the spacecraft p ositions.
ated CME-driven sho cks and a simulation of the in-
These space prob es detect particle intensity increases
jection and transp ort of sho ck-accelerated particles.
which constitute the SEP events. The particle in-
We present an application of this mo del to pro duce
tensity pro les observed by spacecraft take di er-
several \typical" synthetic ux and anisotropy pro-
ent forms dep ending on 1 the heliolongitude of the
les which allows us to delimit the particle e ects
source region with resp ect to the observer lo cation,
under di erent conditions and situations.
2 the strength of the sho ck and its eciency accel-
erating particles, 3 the presence of a seed particle
p opulation sub ject of b eing accelerated, 4 the evo-
Key words: solar proton events; CME; Interplanetary
lution of the sho ck its sp eed, size and shap e, 5 the
Sho cks.
conditions for the propagation of sho ck-accelerated
particles, and 6 the energy considered Cane et al.,
1988; Lario et al., 1998. Particle ux pro les range
1. INTRODUCTION
from a prompt increase shortly after the CME with a
p osterior gradual decay, to a sudden increase shortly
a few hours b efore the arrival of the interplane-
Large solar energetic particle SEP events, charac-
tary sho ck at the spacecraft, passing through gradual
terized by gradual intensity timescales, are generated
and progressing enhancement of the particle intensity
at the sho ck fronts asso ciated with coronal mass ejec-
from the moment of the CME up to the arrival of the
tions CMEs Cane et al., 1988; Kahler et al., 1998.
sho ck see Figure 15 of Cane et al., 1988.
These gradual particle events p ose a serious threat
The simulation of these particle events requires a
to spacecraft comp onents, materials and op erations
knowledge of how particles and sho cks propagate
Turner, 1996. They are characterized by high SEP
through the interplanetary medium, and how sho cks
intensities, rich proton abundances, long time dura-
accelerate and inject particles into interplanetary
tions of the order of several days, and may b e simul-
space. The mo deling of particle uxes and uences
taneously observed over a broad range of heliospheric
asso ciated with SEP events has to consider 1 the
lo cations Reames et al., 1996.
changes in sho ckcharacteristics as it travels through
The injection of energetic particles during gradual
the interplanetary medium, 2 the di erent p oints
events starts when a p erturbation, originated as a
of the sho ck where the observer is connected to, and
consequence of a CME, generates a sho ckwave which
3 the conditions under which particles propagate.
propagates across the solar corona. If the condi-
tions are appropriate this sho ck is able to acceler-
ate particles from the ambient plasma and to inject
2. THE MODEL
them at the base of the interplanetary magnetic eld
IMF lines. These energetic particles stream out
along these lines en route to earth and to the space-
Wehave develop ed a numerical mo del Heras et al.,
craft lo cated in the interplanetary medium. The p er-
1992, 1995; Lario et al., 1998 that repro duces SEP
turbation that generated the sho ck into the corona
6
events by simulating the propagation of the asso- usually detected through in situ observations of so-
ciated interplanetary sho cks and the injection and lar wind plasma and magnetic eld. These measure-
transp ort of sho ck-accelerated particles. In order to ments, made at the lo cation of space prob es, can only
derive the injection rate of sho ck-accelerated parti- give us a few insights ab out the global shap e of the
cles, it is necessary to deconvolve the e ects of the sho ck top ology, but nothing ab out the evolution of
journey of particles from the p oint of the sho ck where its large-scale structure during its journey from the
1
they are accelerated to the observer's p osition. Dur-
-D MHD, self- Sun to the spacecraft. We use the 2
2
ing this propagation, energetic particles su er the
consistent, time-dep endent co de develop ed byWuet
e ects of the IMF and solar wind, that is, fo cus-
al. 1983 as a suitable to ol for studying the evo-
ing, pitch-angle scattering, solar wind convection and
lution of sho cks in the ecliptic plane Dryer, 1994.
adiabatic deceleration e ects. A complete transp ort
This co de gives a dynamical description of the prop-
equation to rst order in v =c, where v is the
sw sw
agation of an interplanetary sho ck between 18 R
constant solar wind velo city which takes into ac-
and 220 R from the Sun. An initial input sho ck
count these e ects is the following Ru olo, 1995:
is considered at 18 R which represents the inter-
planetary sho ck at this distance, and which allows us
to repro duce the arrival times, plasma and magnetic
@F t; ; r;p @
= cos vF
eld data, as well as the sho ck parameters supplied
@t @r
by several spacecraft lo cated at di erent p ositions in
the heliosphere. A mo del describing quantitatively
2
v @
2
the formation of a sho ckwave in the corona from rea-
1 v sec F cos
sw
2
@r c
sonable physical parameters related to observations,
and its evolution to the interplanetary medium, do es
not exist yet. That is b ecause, at present, it is not
v v v @ v
sw sw
2
sec sec 1 F + 1+
p ossible to infer quantitative information concerning
2
@ 2Lr v c
the initial conditions of a sho ck at the corona and
its transition to interplanetary space from the obser-
d @
2
vations made at the onset of CMEs Cane, 1997.
sec 1 F + v cos +
sw
@ dr
Then, what happ ens b elow 18 R remains masked
to our simulation. Injection of particles from the so-
@ @ v v
lar corona or b elow18R accelerated by a di erent
sw
+ ' 1 sec F +
2
evolving coronal sho ck is represented by the mo del
@ @ c
by a Reid-Axford pro le from the ro ot of the IMF
line connecting the observer with the Sun. Once the
sec d @
2 2
sho ck describ ed by the MHD mo del establishes mag-
pv 1 + cos sec F + +
sw
@p 2Lr dr
netic connection with the observer, the injection of
particles is considered from the cobp oint see discus-
+ Qt; ; r;pAr
sion in Lario et al., 1998.
3
d N
where F t; ; r;p = is the density of parti-
dr ddp
cles in a given magnetic ux tub e as a function of
3. APPLICATION OF THE MODEL TO THE
four indep endent variables: t time, pitch-angle
SPACE WEATHER
cosine in the solar wind frame, r helio centric ra-
dial distance, and p momentum in the solar wind
frame. Also v is the particle sp eed, r is the angle
Prediction of particle uxes at di erent heliospheric
between the IMF and the radial direction, Lr is the
lo cations during gradual SEP events requires to know
fo cusing length B=dB =dz , z is the distance along
the characteristics of the evolving sho cks and their ef-
the magnetic eld line dr = dz cos , and ' is
fects on particle p opulation. There is a wide variety
the pitch-angle di usion co ecient. Ar represents
of SEP events and asso ciated sho cks Cane et al.,
the area of the ux tub e at a distance r , and Q the
1988. The contribution of a sho ck to the energetic
injection rate of particles accelerated at the sho ckat
particle p opulation evolves as it moves from the Sun
a given energy. In the upstream region of the sho ck,
to 1 AU and b eyond. In principle, its eciency as an
the IMF can be describ ed by a Parker spiral in a
accelerator of particles is di erent at di erent parts
solar wind steady regime. Pitch-angle di usion co-
of its front and for di erent energies. The strongest
ecient is parameterized following the quasi-linear
parts of a sho ck near its central region are pre-
theory Jokipii, 1971.
sumably more ecient accelerating particles than its
weak anks. When sho cks are close to the Sun, they
The injection of particles is considered to take place
are able to accelerate particles to high energies up to
at the cobp oint Heras et al., 1995, that is the fo ot
energies as high as 1 GeV; Kahler, 1994 but only to
p oint at the sho ck front of the IMF line connecting
lower energies when they are arriving at 1 AU. That
with the observer. All particles injected from the cob-
leads to a softening of the sho ck-accelerated particle
p oint are considered to ll the same ux tub e where
energy sp ectrum while the sho ck propagates b etween
they propagate. As the sho ck expands, the cobp oint
the Sun to farther in the interplanetary medium.
moves along the sho ck front. The instantaneous p o-
sition of the cobp ointisgiven by the intersection b e-
In order to discern the e ect of the di erent factors tween the instantaneous p osition of the sho ck and the
that determine the particle ux of SEP events, the ux tub e where the observer is lo cated.
simulation of a large numb er of particle events is re-
quired. The present state-of-the-art of SEP-event In order to describ e the evolution of sho cks through
simulation is rather reduced see Sanahuja & Lario the interplanetary medium a magnetohydro dynamic
[1998] for a review. In Lario et al. 1998, we MHD mo del is required. Interplanetary sho cks are
7
Figure2. Dependence of the injection rate Q on VR at
di erent energies for the SEP event on 24 April 1979
after a simulation of ISEE-3 observations.
Figure1. Two bottom panels: Evolution of the cobpoint
coordinates heliocentric radial distance and angle with
respect to the Sun-spacecraft line for Helios-2 and ISEE-
3. Top panel: Evolution of VR at both cobpoints. The
origin of time is set at the occurrence of the solar event.
Each line extends from the moment where the simulated
shock and spacecraft establish magnetic connection up to
the arrival of the shock vertical lines at both spacecraft.
1
have repro duced the 50 kev-10 MeV proton ux
and anisotropy pro le of four SEP events asso ciated
with interplanetary sho cks observed by the ISEE-3
Figure3. Low-energy ux pro le derived for Helios-2 as-
spacecraft. These simulations allow us to relate the
suming log Q /VR. Thin lines show the ux pro les mea-
temp oral evolution of the MHD prop erties of sho cks
sured by ISEE-3 and Helios-2. Thick dashed line shows
to the injection rate of sho ck-accelerated particles.
the t for ISEE-3. The thin dashed line shows the ux
From the MHD simulation of the sho ck propagation,
pro le predicted by the model for Helios-2, under the as-
it is p ossible to estimate the MHD strength at each
sumptions commented on in the text. Vertical lines repre-
p oint of its front, and particularly at the cobp oint.
sent the shock passage, and the arrow indicates the time
The strength of the sho ck is characterized by the
of the solar activity.
downstream to upstream normalized velo city ratio,
VR=[V d V u]=V u, where V is the radial
r r r r
plasma velo city and u and d stand for the values up-
stream and downstream of the front, resp ectively,as
considered Q as a free parameter of the simulation.
measured from a xed frame at the Sun. We have
After the simulation, wehave compared the evolution
found a functional dep endence of the injection rate
of Q to the evolution of VR at the cobp oint. Figure
Q with VR for the di erentevents wehave simulated
2 displays logQ versus VR at di erent energies. Each
Lario et al., 1998. Once the prop erties of a sho ck
dot gives a value of VR and Q used for the simulation
in particular VR are known, this dep endence al-
at each temp oral step. Dashed lines are the result
lows us to infer the contribution of the sho cktothe
of linear regressions to each set of p oints. We have
particle p opulation as it travels to 1 AU.
found, as a go o d approximation, a linear dep endence
logQ /VR. This dep endence is di erent at di erent
Let us study an application of such a dep endence.
energies. That is a re ection of the multitude of fac-
The two b ottom panels of Figure 1 show the evolution
tors that may in uence the values of Q at di erent
of the cobp oint p osition as given by the MHD sim-
energies: the presence of a seed particle p opulation to
ulation of the sho ck asso ciated with the SEP event
b e accelerated, the presence of a turbulent foresho ck
on 24 April 1979 see Lario et al., 1998. This sho ck
region whichmay act as a reservoir of particles, the
was observed by the ISEE-3 and Helios-2 spacecraft
dep endence of the mechanism of acceleration on the
Sanahuja et al., 1983. The lo cation of b oth space-
angle which at the present state of the mo del
craft with resp ect to the parent solar activityisin-
Bn
is dicult to compute without large error bars, etc.
dicated by the inset on the top panel of Figure 1.
All these factors mayhave a signi cant e ect on the
Each spacecraft has di erent cobp oints. In the lowest
result shown in Figure 2. In spite of these uncertain-
panel we show the angle between the Sun-cobp oint
ties the dep endence logQ /VR provides us a wayto
and Sun-spacecraft lines, and in the top panel the
relate the MHD prop erties of the sho ck to the injec-
evolution of VR at the cobp oint for b oth spacecraft.
tion rate of sho ck-accelerated particles, and to infer
As the cobp oint moves toward the central part of
once the sho ckisknown the ux pro les at di erent
the sho ck, VR increases indicating a higher velo city
heliospheric p ositions. Lario et al. 1998 apply this
jump across this part of the sho ck front. As the sho ck
idea to predict the proton ux observed by Helios-2
moves away from the Sun it weakens.
after the simulation p erformed for ISEE-3 observa-
tions. Figure 3 shows the observed and simulated
In Lario et al. 1998 wehave pro ceeded to simulate
ux pro les at low energy in two similar energetic
the proton ux and anisotropy pro les observed by
channels of Helios-2 and ISEE-3 for this SEP event.
ISEE-3 for this event at di erent energies. Wehave
As can b e seen, the observed and synthesized pro les
1
also 100 MeV and 70 MeV for two particular events
for Helios-2 t closely well.
8
In Lario et al. 1995 we have pro ceeded in the
same way to pro duce \typical" synthetic ux and
anisotropy pro les characteristic of di erent SEP
events. After the analysis of the most intense
SEP events asso ciated with interplanetary sho cks ob-
served by ISEE-3 between August 1978 and April
1980 Sanahuja & Domingo, 1987 we have con-
sidered an averaged sho ck whose propagation from
the Sun to 1 AU lasts between 45 and 50 hours.
The MHD simulation of such sho ck see Lario et
al. 1995 for details allows us to know VR along
its front and throughout its journey and to deduce
the injection rate Q of sho ck-accelerated particles
through a dep endence logQ /VR. Assuming aver-
age prop erties for particle transp ort see Lario et al.,
1995 we have pro duced di erent synthetic 1-MeV
proton ux and anisotropy pro les at di erent helio-
spheric p ositions. Figure 4 shows those pro les over-
plotted on observations for three SEP events. The
tting of the pro les are surprisingly go o d in spite of
the simplicity of the assumptions made.
4. CONCLUSIONS
Assuming very simple and average conditions we in-
fer a relation that allows us to determine the in-
jection rate of sho ck-accelerated particles from the
MHD conditions at the frontofinterplanetary sho cks
driven by CMEs. The \synthetic" particle ux and
anisotropy pro les built up using this simple relation
can b e used as a to ol to describ e the uence of parti-
cles and its temp oral evolution at a particular helio-
spheric lo cation b efore the o ccurrence of SEP events.
A study of a larger numberofevents is required b e-
fore drawing de nite conclusions.
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Figure4. Flux and anisotropy pro les observed by ISEE-
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