Review of CIR-related Particle Composition, Charge States, & Energy Spectra

51
SHINE 2006 WG2/3 - CIRs & Energetic Particles 1 Review of CIR-related Particle Composition, Charge States, & Energy Spectra Joe Mazur The Aerospace Corporation Glenn Mason Johns Hopkins/APL Joe Dwyer Florida Institute of Technology Mihir Desai Southwest Research Institute

description

Review of CIR-related Particle Composition, Charge States, & Energy Spectra. Joe Mazur The Aerospace Corporation Glenn Mason Johns Hopkins/APL Joe Dwyer Florida Institute of Technology Mihir Desai Southwest Research Institute. Processes for 1 AU observations of solar material. - PowerPoint PPT Presentation

Transcript of Review of CIR-related Particle Composition, Charge States, & Energy Spectra

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Review of CIR-related Particle Composition, Charge States, &

Energy SpectraJoe Mazur

The Aerospace Corporation

Glenn Mason

Johns Hopkins/APL

Joe Dwyer

Florida Institute of Technology

Mihir Desai

Southwest Research Institute

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After Stone et al., Space Sci Rev., 86, 1, 2000

Processes for 1 AU observationsof solar material

SolarPhotospheric

MaterialFractionation

CoronalMaterial

Solar WindAccelerationMechanism

CoronalMass

Ejections

SolarWind

InterplanetaryShock

Acceleration

Accelerationin CorotatingInt. Regions

Transportto 1 AU

Transportto 1 AU

SolarWind

Interpl.Shock

Particles

C I REvents

GradualSEP

Events

1 keV/nuc 1 MeV/nuc 1 GeV/nuc

SW

ISP

C I R

SEP

ShockAcceleration

by CMEs

ImpulsiveSolar Flare

Acceleration

Transportto 1 AU

ImpulsiveSEP

Events

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Desai et al., JGR, 104, 6705, 1999

10-6

10-4

10-2

100

102

104

339 340 341 342 343 344 345

Day of 1994

0.06 MeV/nucleon

0.24 0.95

1.93

2.85

5.6

EPACT / WIND

300

400

500

600

700

800

SWE / WIND

Mason et al., ApJ Letters, 486, L149, 1997

5 AU 1 AU

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0

0.05

0.1

0.15

0.2

0.25

149 150 151 152 153 154 day of 1995

Mg/O ratio

0.1

1

10

100

16O 70 keV/n

Vsw = 666 km/s

Stream interface

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0.4

0.5

0.6

0.7

0.8

0.9

1

1.1

350 400 450 500 550 600 650 700 750

C/O

Solar wind speed (km/s)

In ecliptic SW

Coronal hole SW

Mason et al., ApJ Letters, 486, L149, 1997see also Richardson et al., JGR 98, 13, 1993

Abundances

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0

0.05

0.1

0.15

0.2

350 400 450 500 550 600 650 700 750

Fe/O

Solar wind speed (km/s)

0

0.05

0.1

0.15

0.2

350 400 450 500 550 600 650 700 750

Si/O

Solar wind speed (km/s)

0

0.05

0.1

0.15

0.2

0.25

0.3

350 400 450 500 550 600 650 700 750

Mg/O

Solar wind speed (km/s)

0

0.05

0.1

0.15

0.2

0.25

0.3

0.35

0.4

350 400 450 500 550 600 650 700 750

Ne/O

Solar wind speed (km/s)

0.4

0.5

0.6

0.7

0.8

0.9

1

1.1

350 400 450 500 550 600 650 700 750

C/O

Solar wind speed (km/s)

In ecliptic SW

Coronal hole SW

50

100

150

200

350 400 450 500 550 600 650 700 750

He/O

Solar wind speed (km/s)

Coronal hole SW

In ecliptic SW

Ratios vs. solar wind speed

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Abundance summary

• similar to solar system except for factor of 2-3 enhancement of He and C/O

• increase of He/O, C/O, and Ne/O with solar wind speed

• He abundance increases from 1 to 5 AU

Mason & von Steiger et al. Space Sci. Rev. 89, 1999 (ISSI CIR Workshop held in 1998)

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Ulysses 4.5 AU

Gloeckler et al., JGR, 99, 17637, 1994.

10-9

10-7

10-5

10-3

10-1

101

103

105

107

109

1 10

F(W) Phase Space Density (s

3

/km6)

W Ion Speed (SC frame)/Vsw

HI-SCALE

SWICS

H+He+

He++

He

1991.292.0400-293.04004.485 AU

Pick up ion He+ increases its contribution to CIRs at greater radial distances

Suggested that other pickup ions (such as inner source) at 1 AU might account for some puzzling composition observations

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v’/Vsw1 0-4

1 0-2

1 00

1 02

1 04

1 06

1 1 0

H+

He+

He2+

CIR 1, F’

Chotoo et al., JGR, 105, 23107, 2000.

Acceleration of suprathermal He+

in CIRs: enhanced 103 - 104 over solar wind

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Mobius et al. Geophysical Research Letters, 29, 2001

Mazur et al. ApJ 566, 2002

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Mobius et al. Geophysical Research Letters, 29, 2001

Species SAMPEX ACE

He 2.00±0.12 -

C 4.83±0.27 5.1±0.3

O 6.12±0.37 6.1±0.35

Ne 7.25±0.25 7.8±0.5

Fe 13.00±0.48 10.5±0.6

Mazur et al. ApJ 566, 2002

Averaged CIR charge states: ~0.5 MeV/n

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Möbius et al., AIP Conf. Proc. 598, 201, 2001

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Charge state summary

• More pickup He at 4.5 AU than 1 AI (at 1 AU the pickup He is ~15% He++, while at 4.5 AU it is twice as abundant)

• Heavy ions at 1 AU show little evidence of pickup species

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10-7

10-5

10-3

10-1

101

103

0.01 0.1 1 10

WIND/ STEP & LEMT - SAMPEX / LICA12/6/94 18:00 - 12/7/94 18:00

MeV/nucleon

H

HeCNO

Fe

Mason et al., ApJ Letters, 486, L149, 1997

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SummaryAbundances

Ion composition similar to solar system but with some differencesStill puzzling dependence of some ratios on solar wind speed

Charge statesLittle evidence of Z>2 pickup ions at 1 AULarge abundance of pickup helium at 5 AU

Energy spectraPower law from tens of keV/n to ~1 MeV/nSteepening above ~1 MeV/nSpectral forms do not change out to 10’s of AU

The source population is coming from the suprathermal region, but that population is not just heated solar wind; other constituents are important

Most often the 1 AU particles are not accelerated at shocks requiring another mechanism (Jokipii et al. 2003) As we approach solar minimum we have the opportunity to revisit some of these observables with ACE

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Essential new work needed:

• Complete ACE surveys with much larger number of species identified

• fully characterize properties of suprathermal / pick-up ion distributions

• detailed theoretical models to probe injection issues

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10-7

10-5

10-3

10-1

101

103

105

107

1 10

MASS, STICS, and STEPCIR 2: May 30, 1995 10:00-22:30 UT

Helium Spectra

V/Vsw (SC Frame)

MASS

STICS

STEP

C. Chotoo, Ph.D. thesis, U of Maryland 1998

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10 -39

10 -37

10 -35

10 -33

10 -31

10 -29

10 -27

10 -25

0.001 0.01 0.1 1 10 100

Fisk & Lee 1 AU spectral form vs. distance to shock

1 AU1.5 AU2 AU3 AU4 AU5 AU6 AU

Energy/n

Shock location:

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10-5

10-4

10-3

10-2

10-1

100

101

102

103

0.01 0.1 1 10

WIND/STEP Spectra5/30/95 9:39:04 to 5/31/95 14:19:28

MeV/nucleon

STEP C+N+O Flux

Fisk & Lee (1980) Spectral Form(numerical solution)

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Energy spectra summary

• power law from tens of keV/n to ~1 MeV/n• steepening above ~1 MeV/n• spectral forms do not change out to 10’s of AU

See also Mason & von Steiger et al. Space Sci. Rev. 89, 1999 (ISSI CIR Workshop held in 1998)

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Solar WindAccelerationMechanism

CoronalMass

Ejections

3He-rich Solar Flare

Accelelration

Slow SolarWind

TransientShock

Acceleration

CorotatingInt. Regions

Transportto 1 AU

Transportto 1 AU

SolarWind

ESPEvents

C I REvents

SolarPhotospheric

Material

Fractionation

CoronalMaterial

Fast SolarWind

InterstellarPick up

Ions

InnerSource(dust?)

Q = 1pick up

ions

Transportto 1 AU

3He-richSEP

Events

InterplanetarySuprathermal Ions

Transportto 1 AU

C M EAssocSEPs

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Energy spectra summary

• More pickup He at 4.5 AU than 1 AI (at 1 AU the pickup He is ~15% He++, while at 4.5 AU it is twice as abundant)

• Heavy ions at 1 AU show little evidence of pickup species

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23Möbius et al., AIP Conf. Proc. 598, 201, 2001

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24Möbius et al., AIP Conf. Proc. 598, 201, 2001

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25Richardson et al., JGR, 98, 13, 1993

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C N Ne Mg Si S Fe0.01

0.10

1.00shock

CIR

solar wind

Dwyer et al, in preparation, 2002

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Fisk & Lee acceleration model--

• particles in CIRs accelerated by compression at forward and reverse shocks at several AU: propagate in to 1 AU

• adiabatic deceleration in solar wind included• yields distribution function spectra and gradients similar to

observations above ~100 keV/n• injection energy > 5 keV required, ie from postulated

suprathermal tail of the solar wind• composition similar to source material (assumed to be solar

wind suprathermal tail) -- (note: no systematic measurements of solar wind comp. available at that time)

L. A. Fisk and M. A. Lee, Astrophys. J., 237, 620, 1980

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Suprathermals as a seed population--

• SEP related events– “super events” in the inner solar-system (Dröge et al. 1992.)– Peak intensities in August 1972 (Smart et al. 1990)

• Interplanetary shocks– Aug 1978 shock (Gosling et al. 1981)

– IP shock survey (Tsurutani & Lin 1985)

• Sources?

– long lived remnants of solar flares

– planetary bow shocks

– corotating interaction regions

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Fisk & Lee CIR spectral form--

CIR spectral form:

where: v = particle speed; r = radius of observer; rs = shock radius;

= shock strength; diffusion coefficientV = solar wind speed

f =

r

rs

⎜⎞

2 / ( 1 − ) + V / ( o

v )

v− 3 / ( 1 − )

exp −

6 o

v

V ( 1 − )2

⎜⎞

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CIR model status 1970s-80s

• Successful:– spectra above ~100 keV/n

– composition “similar” to (unmeasured) solar wind

– origin at several AU, and gradients

• Not successful / unaddressed:– C/O ratio

– spectral forms vs. compression ratios

– intensities

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New CIR energetic particle observations & challenges to standard model--

• Particle spectra continue to rise down to ~10 keV/nucleon at 1 AU

• C/O ratio dependence on solar wind speed• Mg/O shows no FIP effect • large abundance of He+ at 1 and several AU• 3He abundance enhanced compared to solar wind

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0.05

0.1

0.15

pre-FS FS to SI SI to RS post-RS

Solar Wind Mg/O Abundance Variations in CIRsSWICS/ Ulysses: 15 CIRs (4.5 - 5.4 AU)

Mg/O

from: Wimmer-Schweingruber et al., JGR vol 102, 17407,1997

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34Hilchenbach et al., Trnas. Am.Geophys. U., 78, F554, 1997

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Interstellar Gas Flow in Inner Solar System

From: University of New Hampshire group WWW pagehttp://www-ssg.sr.unh.edu/tof/Missions/Ace/aceset.html

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0.01

0.1

1

10

100

103

1 3 5 7 9 11 13

Seasonal Variation of CIR abundances(filled circles = STEP; open circles = LICA)He/O

C/ONe/O4He/OC/ONe/O

Month of Year

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2 3 4 5 6mass (nucleons)

0

100

200

300

3He/4He =0.0016 ± 0.0002

ACE/ULEIS 0.4-1.0 MeV/nsum of 6 CIRs

Dwyer et al, in preparation, 2002

3He is enriched in CIRs -- about 4 times the solar wind value compared to 4He

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Role of pick up ions --

• consistent with He+ abundance• tempting explanation for C/O ratio, but

– no seasonal variation of heavy ion abundances detected, but data is sparse

– at 1 AU C+ is a small fraction of CIR carbon

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39Gloeckler & Geiss, Space Sci. Rev, 86, 127, 1998CY 1994, <r> = 2.8AU; <latitude> = -65°<vsw>=784 km/s

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10

-1

10

0

relative flux

(a) CIR

He

O

Fe

10

-1

10

0

60 62 64 66 68 70

relative flux

adjusted invariant latitude

(b) SEP

HeO

Fe

Mazur, Mason & Mewaldt, 2002, ApJ, in press

SAMPEX:

geomagnetic latitude cutoffs of:

(a) 14 CIRs (1992- 95), and

(b) all 1998 SEP events

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10

1

10

2

10

3

62 63 64 65 66 67

Rigidity (MV)

adjusted invariant latitude

He

C

O

Ne

Fe

Fe

Ne

O

C

He SEP

CIR

Mazur, Mason & Mewaldt, 2002, ApJ, in press

SAMPEX:

Calibration of adjusted magnetic invariant latitude cutoffs for CIRs and SEP events

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10

-3

10

-2

10

-1

10

0

carbon

C

+1

10

-3

10

-2

10

-1

10

0

oxygen

O

+1

flux (#/cm

2

-sec-sr-MeV/n)

10

-3

10

-2

10

-1

10

0

55 60 65 70 75

adjusted invariant latitude

neon

Ne

+1

Mazur, Mason & Mewaldt, 2002, ApJ, in press

SAMPEX:

Observed magnetic cutoffs for CIR events, vs inferred cutoff if ions were singly ionized.

Singly stripped ions must be no more than a few percent of total.

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CIR abundance details show that bulk solar wind source does not fit the new observations--

• Source population is coming from suprathermal region, but that population is not just heated solar wind -- other constituents important

• Do other shock-associated energetic particle observations show evidence for suprathermal seed ions? YES: SEPs, ESPs -- tracer ion is 3He

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10

-4

10

-3

10

-2

10

-1

10

0

10

1

10

2

155 156 157 158 159 160

ACE / ULEIS 0.7 MeV/nucleon

Day of 1999

4

He

3

He

2B N17W69

Mason et al., Ap.J. Letters, 525, L133, 1999

3He and 4He time intensity profiles in large June 4, 1999 solar particle event

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Enhanceed abundances of 3He in large SEP events

ACE/SIS 8-13 MeV/n

0

2,000

4,000

6,000

8,000

10,000

12,000

14,000

0

20

40

60

80

100

120

140

2 3 4 5 6

Mass (AMU)

(a)

"finite" 3He

ACE/ULEIS 0.5-2 MeV/n

Wiedenbeck et al., AIP Conf Proc 528, 107, 2000Mason et al., Ap.J. Letters, 525, L133, 1999

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Suprathermals show 10-100 times more variation in intensity than solar wind -- likely critical issue in energetic particle intensities

0.01

0.1

1

10

100

1000

50 70 90 110 130 150

WIND / EPACT / STEP30 keV/n Fe

Day of 2000

104

105

106

107

108

109

50 70 90 110 130 150

WIND / SWENp * Vsw ^2

Day of 2000

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Conclusions: 1 AU CIRs• CIR source is not bulk solar wind, but rather the

suprathermal region (v/vsw >~ 1.5)• time dependent, multiple ingredients:

• solar wind suprathermal tail

• pick up ions (interstellar)

• pick up ions (inner source)

• other remnants (large SEP events, impulsive SEP events)

• at < few hundred keV/n, CIR ions are “locally accelerated”

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200

300

400

500

600

700

800

900

1000

10 20 30 40 50 60

ACE / SWEPAM solar wind speed

SWEPAM Vsw

Day of 2000

0.001

0.01

0.1

1

10

10 20 30 40 50 60

ACE / ULEIS 270 keV/nucleon

C12 0.2731 MeV/nuc O16 0.2731 MeV/nuc

Day of 2000

27 daysCIRCIR CIRSEP

CIRs observed in early 2000 on ACE

•typical appearance

•note change in C/O ratio in CIRs vs. solar events

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10

100

1000

10 4

10 20 30 40 50 60

ACE / ULEIS E> 200 keV/nCIR and SEP mass histograms

tof_mass -- cir tof_mass -- SEP renormalized

Mass (AMU)

2/6/2002

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100

1000

10 4

10 15 20 25 30

ACE / ULEIS E> 200 keV/nCIR and SEP mass histograms

tof_mass -- cir tof_mass -- SEP renormalized

Mass (AMU)

2/6/2002

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Introduction

• Dependence of some abundances on coronal hole speed• No reflection of solar wind abundance changes across stream interface

- pointing to another source (the suprathermals) / Ubiquitous tails • Little influence of Z>2 pickup ions at 1 AU• Most 1 AU events don’t have shocks• complicated time profile that includes local acceleration and transport of

ions from shocks later in the events, as long as a week (Reames)