interplanetary coronal mass ejections from messenger...

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Interplanetary Coronal Mass Ejections from MESSENGER Orbital Observations at Mercury Reka M. Winslow 1 , Noé Lugaz 1 , Lydia C. Philpott 2 , Nathan A. Schwadron 1 , Charles J. Farrugia 1 , Brian J. Anderson 3 , and Charles W. Smith 1 (1) Institute for the Study of Earth, Oceans, and Space, University of New Hampshire ([email protected]), (2) Earth, Ocean and Atmospheric Sciences, University of British Columbia, (3) John Hopkins University Applied Physics Laboratory. Poster based on: Winslow, R. M. et al. (2015), Interplanetary coronal mass ejections from MESSENGER orbital observations at Mercury, J. Geophys. Res. Space Physics, 120, doi:10.1002/2015JA021200. SH53A-2469 AGU Fall Meeting 2015 1. Summary • Used observations from MESSENGER in orbit around Mercury to study interplanetary coronal mass ejections (ICMEs) near 0.3 AU. Cataloged over 60 ICMEs at Mercury between 2011 - 2014. Investigated key ICME property changes from Mercury to 1 AU. Find: Good agreement with previous studies for magnetic field strength dependence on dis- tance, and evidence that ICME deceleration con- tinues past the orbit of Mercury. This ICME database useful for multipoint spacecraft studies of recent ICMEs, as well as for model validation of ICME properties. 2. ICME Identification ICMEs identified using magnetic field measure- ments only, due to lack of solar wind data with MES- SENGER. Strict selection criteria: a) interplanetary shock observed b) shock followed by sheath and magnetic ejecta c) event lasted for the duration of at least 1 MES- SENGER orbit through Mercury’s magnetosphere d) event caused a visible distortion of the magneto- sphere Selection criteria biases towards fast ICMEs that are shock-driving and ICMEs with magnetic cloud- like characteristics. Also determined corresponding CME counter- part at the Sun for each event. Example ICME: 3. ICME Properties at Mercury • ICME speed estimated from CME ejection time at the Sun, arrival time at Mercury, and Mercury’s heliocentric distance. -> This average speed is likely a maximum speed of the ICME at MESSENGER. • Maximum ICME |B| observed is 310 nT. • Fastest transit time from Sun to Mercury was 6 hr, longest transit time 52 hr. • Fastest transit speed 2350 km/s, slowest transit speed 325 km/s. • Large spread in transit times and speeds indicates that due to proximity to Sun, MESSENGER observed a wide range of ICMEs, even ones that may be too slow or small to be detected at 1 AU. 4. Differences in ICME Properties Between Mercury and 1 AU • Used existing databases of ICMEs at 1 AU for the same time period. Main Results: , in good agreement with previous studies. • ICME deceleration continues beyond the orbit of Mercury: (1) Shallow speed decrease with distance, (2) Average transit time from Sun to Mercury 20% faster than expected based on average transit times to 1 AU, (3) Significantly shallower ICME transit time dependence on initial CME speed observed at 1 AU compared to predictions based on MESSENGER ICME catalog. ICME magnetic shock compression ratio higher at MESSENGER (1.97) than at STEREO (1.64). ICME deceleration may explain the lower mean shock compression at 1 AU compared to that at Mercury. 5. Example ICME: 12 July 2012 Event • Observed by MESSENGER and ACE • Illustrates that this ICME database can be used for both model validation and propagation studies of events observed in conjunction. • Some of the large-scale structure is retained in propagation (B R stongly negative at both distances) • Non-dimensional expansion rate of the cloud con- firmed by two separate methods at Mercury and ACE to be: • Compare to model predictions of Hess & Zhang [2014] for this event, which fit remote-sensing ob- servation a posteriori to the semi-empirical drag model of Vrsnak et al. [2013]. • Model does quite well at estimating sheath size and arrival time at Mercury: 0 50 100 150 200 250 300 0 5 10 15 Max |B| in ME (nT) No. of ICMEs Mean = 86.2±5.0 0 50 100 150 200 250 300 350 0 5 10 15 Max |B| in Sheath (nT) No. of ICMEs Mean = 84.6±5.8 0 10 20 30 40 50 60 0 5 10 15 Shock transit time (hours) No. of ICMEs Mean = 23.0±1.1 0 10 20 30 40 50 60 0 5 10 15 ME transit time (hours) No. of ICMEs Mean = 25.6±1.2 0 500 1000 1500 2000 2500 0 5 10 15 Shock Transit Speed (km/s) No. of ICMEs Mean = 792±45 0 500 1000 1500 2000 2500 0 5 10 15 ME Transit Speed (km/s) No. of ICMEs Mean = 706±41 0 0.2 0.4 0.6 0.8 0 5 10 15 ME radial size (AU) No. of ICMEs Mean = 0.223±0.018 0 0.05 0.1 0.15 0.2 0 5 10 15 Sheath radial size (AU) No. of ICMEs Mean = 0.0434±0.0036 a) b) 0.2 0.3 0.4 0.5 0.6 0.7 0.8 0.9 1 1.1 0 50 100 150 200 250 300 Heliocentric Distance (AU) ME Mean |B (nT) | MESSENGER+ACE data <B> = 10.9 r -1.85 ; Gulisano et al. (2010) <B> = 18.1 r -1.64 ; Leitner et al. (2007) <B> = 8.3 r -1.52 ; Wang et al. (2005) <B> = e (2.01+/-0.15) r (-1.95+/-0.19) 0.2 0.3 0.4 0.5 0.6 0.7 0.8 0.9 1 1.1 0 50 100 150 200 250 300 ME maximum |B| (nT) MESSENGER+STEREO data Bmax = e (2.5+/-0.06) r (-1.89+/-0.14) Bmax = 17.7 r -1.73 ; Farrugia et al. (2005) Heliocentric Distance (AU) 0 500 1000 1500 2000 2500 0 50 100 150 200 250 300 350 Shock transit speed (km/s) Maximum |B| in the ICME (nT) MESSENGER data; |B| = 0.03 v + 59.5 cc = 0.55 0.2 0.4 0.6 0.8 1 0 500 1000 1500 2000 2500 Maximum Shock Speed (km/s) Heliocentric Distance (AU) MESSENGER+ACE data |v| = e (6.14+/-0.05) r (-0.45+/-0.09) 0.2 0.4 0.6 0.8 1 0 500 1000 1500 2000 2500 Maximum ME Speed (km/s) MESSENGER+STEREO data |v| = e (6.18+/-0.04) r (-0.26+/-0.08) a) b) Heliocentric Distance (AU) 0 500 1000 1500 2000 2500 0 25 50 75 100 125 150 Coronal Speed (km/s) ME Transit Time (hrs) Sun to Mercury Predicted Sun to 1 AU TT = e (9.37+/-0.79) v (-0.78+/-0.12) TT = e (7.92+/-1.2) v (-0.71+/-0.17) a) b) 0 500 1000 1500 2000 2500 0 25 50 75 100 125 150 Coronal Speed (km/s) Shock Transit Time (hrs) Sun to Mercury Predicted Sun to 1 AU TT = 441 v -0.29 ; Vrsnak & Zic (2007) TT = e (9.08+/-0.83) v (-0.76+/-0.12) TT = e (7.75+/-1.2) v (-0.704+/-0.17) 0 5 10 15 20 25 30 35 40 45 50 0 25 50 75 100 125 150 175 200 225 Transit time (hours) Radial distance (R Sun ) Shock drag model - Hess & Zhang (2014) Ejecta drag model - Hess & Zhang (2014) MESSENGER shock transit time MESSENGER ejecta transit time 0 5 10 15 20 25 30 35 40 45 50 0 5 10 15 20 25 30 35 40 45 50 Transit time (hours) Standoff distance (R Sun ) Drag model - Hess & Zhang (2014) MESSENGER standoff distance a) b) High ICME |B| -> high ICME speed? B Total (nT) 0 15 30 45 60 75 B R (nT) -75 -50 -25 0 25 50 75 B T (nT) -75 -50 -25 0 25 50 75 UTC 12/30 16:48 12/30 19:12 12/30 21:36 12/31 00:00 12/31 02:24 12/31 04:48 12/31 07:12 12/31 09:36 B N (nT) -75 -50 -25 0 25 50 75 10 12 10 11 10 10 H + (Scan Total)

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Interplanetary Coronal Mass Ejections from MESSENGER Orbital Observations at MercuryReka M. Winslow1, Noé Lugaz1 , Lydia C. Philpott2 , Nathan A. Schwadron1 , Charles J. Farrugia1 , Brian J. Anderson3, and Charles W. Smith1

(1) Institute for the Study of Earth, Oceans, and Space, University of New Hampshire ([email protected]), (2) Earth, Ocean and Atmospheric Sciences, University of British Columbia, (3) John Hopkins University Applied Physics Laboratory.

Poster based on: Winslow, R. M. et al. (2015), Interplanetary coronal mass ejections from MESSENGER orbital observations at Mercury, J. Geophys. Res. Space Physics, 120, doi:10.1002/2015JA021200.

SH53A-2469AGU Fall Meeting 2015

1. Summary

• Used observations from MESSENGER in orbit around Mercury to study interplanetary coronal mass ejections (ICMEs) near 0.3 AU.

• Cataloged over 60 ICMEs at Mercury between 2011 - 2014.

• Investigated key ICME property changes from Mercury to 1 AU.

Find: • Good agreement with previous studies for magnetic field strength dependence on dis-tance, and evidence that ICME deceleration con-tinues past the orbit of Mercury.

• This ICME database useful for multipoint spacecraft studies of recent ICMEs, as well as for model validation of ICME properties.

2. ICME Identification

• ICMEs identified using magnetic field measure-ments only, due to lack of solar wind data with MES-SENGER.

• Strict selection criteria: a) interplanetary shock observedb) shock followed by sheath and magnetic ejectac) event lasted for the duration of at least 1 MES-SENGER orbit through Mercury’s magnetosphered) event caused a visible distortion of the magneto-sphere

• Selection criteria biases towards fast ICMEs that are shock-driving and ICMEs with magnetic cloud-like characteristics.

• Also determined corresponding CME counter-part at the Sun for each event.Example ICME:

3. ICME Properties at Mercury

• ICME speed estimated from CME ejection time at the Sun, arrival time at Mercury, and Mercury’s heliocentric distance. -> This average speed is likely a maximum speed of the ICME at MESSENGER.

• Maximum ICME |B| observed is 310 nT.

• Fastest transit time from Sun to Mercury was 6 hr, longest transit time 52 hr.

• Fastest transit speed 2350 km/s, slowest transit speed 325 km/s.

• Large spread in transit times and speeds indicates that due to proximity to Sun, MESSENGER observed a wide range of ICMEs, even ones that maybe too slow or small to be detected at 1 AU.

4. Differences in ICME Properties Between Mercury and 1 AU

• Used existing databases of ICMEs at 1 AU for the same time period.

Main Results: , in good agreement with previous studies.

• ICME deceleration continues beyond the orbit of Mercury: (1) Shallow speed decrease with distance, (2) Average transit time from Sun to Mercury 20% faster than expected based on average transit times to 1 AU, (3) Significantly shallower ICME transit time dependence on initial CME speed observed at 1 AU compared to predictions based on MESSENGER ICME catalog.

• ICME magnetic shock compression ratio higher at MESSENGER (1.97) than at STEREO (1.64). ICME deceleration may explain the lower mean shock compression at 1 AU compared to that at Mercury.

5. Example ICME: 12 July 2012 Event

• Observed by MESSENGER and ACE

• Illustrates that this ICME database can be used for both model validation and propagation studies of events observed in conjunction.

• Some of the large-scale structure is retained in propagation (B

R stongly negative at both distances)

• Non-dimensional expansion rate of the cloud con-firmed by two separate methods at Mercury and ACE to be:

• Compare to model predictions of Hess & Zhang [2014] for this event, which fit remote-sensing ob-servation a posteriori to the semi-empirical drag model of Vrsnak et al. [2013].

• Model does quite well at estimating sheath size and arrival time at Mercury:

0 50 100 150 200 250 3000

5

10

15

Max |B| in ME (nT)

No. o

f ICM

Es

Mean = 86.2±5.0

0 50 100 150 200 250 300 3500

5

10

15

Max |B| in Sheath (nT)

No. o

f ICM

Es

Mean = 84.6±5.8

0 10 20 30 40 50 600

5

10

15

Shock transit time (hours)

No. o

f ICM

Es

Mean = 23.0±1.1

0 10 20 30 40 50 600

5

10

15

ME transit time (hours)

No. o

f ICM

Es

Mean = 25.6±1.2

0 500 1000 1500 2000 25000

5

10

15

Shock Transit Speed (km/s)

No. o

f ICM

Es

Mean = 792±45

0 500 1000 1500 2000 25000

5

10

15

ME Transit Speed (km/s)

No. o

f ICM

Es

Mean = 706±41

0 0.2 0.4 0.6 0.80

5

10

15

ME radial size (AU)

No. o

f ICM

Es

Mean = 0.223±0.018

0 0.05 0.1 0.15 0.20

5

10

15

Sheath radial size (AU)

No. o

f ICM

Es

Mean = 0.0434±0.0036

a) b)

0.2 0.3 0.4 0.5 0.6 0.7 0.8 0.9 1 1.10

50

100

150

200

250

300

Heliocentric Distance (AU)

ME

Mean |B

(n

T)

|

MESSENGER+ACE data

<B> = 10.9 r−1.85

; Gulisano et al. (2010)

<B> = 18.1 r−1.64

; Leitner et al. (2007)

<B> = 8.3 r−1.52

; Wang et al. (2005)

<B> = e(2.01+/−0.15)

r(−1.95+/−0.19)

0.2 0.3 0.4 0.5 0.6 0.7 0.8 0.9 1 1.10

50

100

150

200

250

300M

E m

axim

um

|B

| (n

T)

MESSENGER+STEREO data

Bmax = e(2.5+/−0.06)

r(−1.89+/−0.14)

Bmax = 17.7 r−1.73

; Farrugia et al. (2005)

Heliocentric Distance (AU)

0 500 1000 1500 2000 25000

50

100

150

200

250

300

350

Shock transit speed (km/s)

Maxim

um

|B

| in

the IC

ME

(nT

)

MESSENGER data;

|B| = 0.03 v + 59.5

cc = 0.55

0.2 0.4 0.6 0.8 10

500

1000

1500

2000

2500

Ma

xim

um

Sh

ock S

pe

ed

(km

/s)

Heliocentric Distance (AU)

MESSENGER+ACE data

|v| = e(6.14+/−0.05)

r(−0.45+/−0.09)

0.2 0.4 0.6 0.8 10

500

1000

1500

2000

2500

Ma

xim

um

ME

Sp

ee

d (

km

/s)

MESSENGER+STEREO data

|v| = e(6.18+/−0.04)

r(−0.26+/−0.08)

a) b)

Heliocentric Distance (AU)

0 500 1000 1500 2000 25000

25

50

75

100

125

150

Coronal Speed (km/s)

ME

Tra

nsit T

ime

(h

rs)

Sun to Mercury

Predicted Sun to 1 AU

TT = e(9.37+/−0.79)

v(−0.78+/−0.12)

TT = e(7.92+/−1.2)

v(−0.71+/−0.17)

a) b)

0 500 1000 1500 2000 25000

25

50

75

100

125

150

Coronal Speed (km/s)

Shock T

ransit T

ime (

hrs

)

Sun to Mercury

Predicted Sun to 1 AU

TT = 441 v−0.29

; Vrsnak & Zic (2007)

TT = e(9.08+/−0.83)

v(−0.76+/−0.12)

TT = e(7.75+/−1.2)

v(−0.704+/−0.17)

0 5 10 15 20 25 30 35 40 45 500

25

50

75

100

125

150

175

200

225

Transit time (hours)

Rad

ial d

ista

nce

(RS

un)

Shock drag model − Hess & Zhang (2014)Ejecta drag model − Hess & Zhang (2014)MESSENGER shock transit timeMESSENGER ejecta transit time

0 5 10 15 20 25 30 35 40 45 500

5

10

15

20

25

30

35

40

45

50

Transit time (hours)

Sta

ndof

f dis

tanc

e (R

Sun

)

Drag model − Hess & Zhang (2014)MESSENGER standoff distance

a) b)

High ICME |B| -> high ICME speed?

UTC12/30 16:48 12/30 19:12 12/30 21:36 12/31 00:00 12/31 02:24 12/31 04:48 12/31 07:12

B Tota

l (nT)

01530456075

UTC12/30 16:48 12/30 19:12 12/30 21:36 12/31 00:00 12/31 02:24 12/31 04:48 12/31 07:12

B R (nT)

-75-50-25

0255075

UTC12/30 16:48 12/30 19:12 12/30 21:36 12/31 00:00 12/31 02:24 12/31 04:48 12/31 07:12

B T (nT)

-75-50-25

0255075

UTC12/30 16:48 12/30 19:12 12/30 21:36 12/31 00:00 12/31 02:24 12/31 04:48 12/31 07:12 12/31 09:36

B N (nT)

-75-50-25

0255075

1012

1011

1010 H+ (

Scan

Tot

al)