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International Symposium on Solar Terrestrial Physics ASI Conference Series, 2013, Vol. 10, pp 11 – 24 Edited by N. Gopalswamy, S. S. Hasan, P. B. Rao and Prasad Subramanian STEREO and SOHO contributions to coronal mass ejection studies: Some recent results N. Gopalswamy * Solar Physics Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA Abstract. This paper summarizes some recent results on coronal mass ejections (CMEs) obtained from the Solar Terrestrial Relations Observatory (STEREO) that relate to previous results from the Solar and Heliospheric Observatory (SOHO). Making use of the extended field of view of the STEREO instruments and the capability to view solar eruptions from vantage points away from the Sun-Earth line, this paper addresses CME morphology and the early evolution of CMEs including shock for- mation indicated by type II radio bursts and EUV disturbances. In situ ob- servations from STEREO locations and Sun-Earth L1 are used to provide evidence to support the idea that all CMEs in the interplanetary medium may be flux ropes. Finally, the use of shock-flux rope morphology to de- termine the heliospheric magnetic field is discussed. Keywords : coronal mass ejections – flux rope – interplanetary CMEs – Sun 1. Introduction Although the coronal mass ejection (CME) phenomenon was discovered in 1971, CME observations were rather limited until the Large Angle and Spectrometric Coro- nagraph (LASCO, Brueckner et al. 1995) on board the Solar and Heliospheric Obser- vatory (SOHO) became operational in 1996. LASCO instruments provided the most extensive and uniform data on CMEs. The number of CMEs observed by SOHO is an order of magnitude higher than the combined number from all pre-SOHO observa- tions (Gopalswamy et al. 2009a). In fact, most of the knowledge on CMEs and their impact on geospace environment accumulated over the past decade can be attributed to SOHO. SOHO observes from the Sun-Earth Lagrange point L1, which is ideal for * email: [email protected]

STEREO and SOHO contributions to coronal mass ejection ...astron-soc.in/bulletin/asics_vol010/011_gopalswamy.pdf · email:[email protected]. 12 N. Gopalswamy observing CMEs

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Page 1: STEREO and SOHO contributions to coronal mass ejection ...astron-soc.in/bulletin/asics_vol010/011_gopalswamy.pdf · email:nat.gopalswamy@nasa.gov. 12 N. Gopalswamy observing CMEs

International Symposium on Solar Terrestrial PhysicsASI Conference Series, 2013, Vol. 10, pp 11 – 24Edited by N. Gopalswamy, S. S. Hasan, P. B. Rao and Prasad Subramanian

STEREO and SOHO contributions to coronal massejection studies: Some recent results

N. Gopalswamy∗Solar Physics Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA

Abstract. This paper summarizes some recent results on coronal massejections (CMEs) obtained from the Solar Terrestrial RelationsObservatory (STEREO) that relate to previous results from the Solar andHeliospheric Observatory (SOHO). Making use of the extended field ofview of the STEREO instruments and the capability to view solar eruptionsfrom vantage points away from the Sun-Earth line, this paper addressesCME morphology and the early evolution of CMEs including shock for-mation indicated by type II radio bursts and EUV disturbances. In situ ob-servations from STEREO locations and Sun-Earth L1 are used to provideevidence to support the idea that all CMEs in the interplanetary mediummay be flux ropes. Finally, the use of shock-flux rope morphology to de-termine the heliospheric magnetic field is discussed.

Keywords : coronal mass ejections – flux rope – interplanetary CMEs –Sun

1. Introduction

Although the coronal mass ejection (CME) phenomenon was discovered in 1971,CME observations were rather limited until the Large Angle and Spectrometric Coro-nagraph (LASCO, Brueckner et al. 1995) on board the Solar and Heliospheric Obser-vatory (SOHO) became operational in 1996. LASCO instruments provided the mostextensive and uniform data on CMEs. The number of CMEs observed by SOHO isan order of magnitude higher than the combined number from all pre-SOHO observa-tions (Gopalswamy et al. 2009a). In fact, most of the knowledge on CMEs and theirimpact on geospace environment accumulated over the past decade can be attributedto SOHO. SOHO observes from the Sun-Earth Lagrange point L1, which is ideal for

∗email: [email protected]

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observing CMEs propagating orthogonal to the Sun-Earth line, but not the halo CMEs(Howard et al. 1982). SOHO did observe hundreds of halo CMEs that propagated inthe direction of Earth or in the anti-Earth direction (Gopalswamy et al. 2010), butthe problem is the occulting disks of the coronagraphs block the Earth-arriving partof the CMEs. This problem is common to all coronagraphs observing from the Sun-Earth line. The twin spacecraft on board the Solar Terrestrial Relations Observatory(STEREO) observe the Sun from various angles with respect to the Sun from theecliptic plane (Kaiser et al. 2008). Combined with the Earth view provided by SOHO,the two views from STEREO provided direct evidence for the three-dimensional na-ture of CMEs (Liewer et al. 2013; Mierla et al. 2011). STEREO’s expanded field ofview both closer to and away from the Sun helped confirm and clarify many SOHOresults. The inner coronagraph COR1 of the Sun Earth Connection Coronal and He-liospheric Investigation suite (SECCHI, Howard et al. 2008) observes down to 1.4Rs and the Extreme Ultra Violet Instrument (EUVI) down to the solar surface. TheHeliospheric Imagers (HIs) observe CMEs over the entire Sun-Earth distance. Ob-servations closer to the Sun with an increased image cadence helped determine theearly kinematics of CMEs (Gopalswamy et al. 2009b; Bein et al. 2011), wave na-ture of EUV disturbances (Gopalswamy et al. 2009c; Veronig et al. 2010), height ofshock formation in the corona (Gopalswamy et al. 2013a,b), and high-latitude CMEs(Gopalswamy 2013). The HI observations helped identify CIRs in white light (Shee-ley et al. 2008; Rouillard et al. 2010), CME tracking in the inner heliosphere (Liu etal. 2010; Möstl et al. 2012; Lugaz et al. 2012), and CME-shock dynamics in the inter-planetary medium (Maloney & Gallagher 2011; Poomvises et al. 2012). Multipointobservations have also helped understand particle propagation. This paper summa-rizes a few of these STEREO results in the backdrop of SOHO results.

2. Basic morphology of CMEs

2.1 Halo CMEs

One of the important morphological features that gained importance during the SOHOera is the halo CME. When Howard et al. (1982) discovered the phenomenon, theycorrectly guessed the reason for the halo appearance: a three-dimensional cone-likeobject projected on to the sky plane and hence appears to surround the occulting disk.Even though hundreds of halo CMEs were observed by SOHO, the 3D structure hadto be inferred only based on similar CMEs from the same active region (Gopalswamy2004; Gopalswamy et al. 2010a). The two views of STEREO provided direct evi-dence that a halo CME appears as a normal CME when viewed broadsided. Figure 1shows the 26 April 2008 CME—one of the first halos observed by SECCHI/COR1.The CME was observed simultaneously by the two STEREO spacecraft (separatedby about 50◦) and SOHO. The EUV images from STEREO and SOHO show thesolar source of the CME as an elongated post eruption arcade in Fig. 1. In STEREOAhead (SA) view, the source was located at N08E33, whereas it was a disk event inSTEREO Behind (SB) view (N08W15) and LASCO view (N08E09). Accordingly,

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STEREO and SOHO CME studies 13

Figure 1. Two views of the 2008 April 26 CME: STEREO-Behind (SB) and STEREO-Ahead(SA). The solar source is shown encircled in the EUV image superposed on COR1 images. TheCME (between solid arrows) and the shock disturbance (between dashed arrows) are shown(from Gopalswamy et al. 2010b).

the CME appeared as a halo CME in SB and LASCO views and as a normal CME inSA view. The speeds measured in the images of the three coronagraphs differ becauseof projection effects and field of view limitations (Gopalswamy et al. 2009b). Themultiple views also help us identify the radial structure of the CME: the main body(flux rope) surrounded by a diffuse disturbance identified as the white-light signatureof the shock (Sheeley et al. 2000; Vourlidas et al. 2003; Gopalswamy et al. 2009b;Ontiveros & Vourlidas 2009; Gopalswamy & Yashiro 2011). Note that the halo CMEcorresponds to the outermost disturbance. Another example of a halo CME is dis-cussed in Section 2.2.

2.2 Expansion and Radial Speeds of CMEs

An issue closely related to the internal structure of CMEs is the flux rope nature. Theflux rope structure appears contradictory to the cone model of CMEs (see e.g., Xieet al. 2004). Gopalswamy et al. (2009d) suggested that the cone model is applicablewhen the CME legs are fat so that the edge-on and face-on widths become compara-ble. Under these circumstances, one can use the cone model to derive the radial speedof CMEs based on sky-plane measurements because the radial (Vrad) and expansion(Vexp) speeds of CMEs are related (Schwenn et al. 2005), but the exact relationshipdepends on the geometry of the cone and the width of the CMEs (Gopalswamy et al.2009d). In other words, Vrad = f (w)Vexp, where f (w) is a function of the half angleof the CME cone (w) and the cones type (flat cone, partial ice-cream cone and fullice-cream cone). For halo CMEs, what is measured in the sky plane is just half ofVexp. Unfortunately, w is unknown for a halo CME, so it is difficult to estimate theradial speed for such CMEs from a single view. From multiple views available fromthe STEREO mission, it is possible to measure w and hence confirm the Vrad − Vexp

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Table 1. Comparison between observations and theory for the 2011 February 15 CME.

Model F(w) Vrad Dev (SA) Dev (SB)Full 1.14 1023 7.6% 3.4%Partial 0.81 727 30% 46%Flat 0.64 574 65% 84%Empirical 0.88 789 20% 34%

relation. We demonstrate this using the 2011 February 15 CME, which was observedas a halo by SOHO and as a limb CME by SA and SB (see Fig. 2(a–c)). Vexp (897kms−1—Fig. 2d) and Vrad (945 kms−1 in SA and 1058 kms−1 in SB—Fig. 2e) weredirectly measured in the sky plane (Gopalswamy et al. 2012b). SOHO and STEREOwere in quadrature during these observations, so the projection effects were mini-mal. In the SA and SB field of view (FOV), the CME full width was also measureddirectly as ∼ 76◦. Fig. 2f shows f (w) for the three types of cones: full ice-creamcone [ f (w) = 1/2(1 + cotw)], partial ice-cream cone [ f (w) = 1/2cosecw] and flatcone [ f (w) = 1/2cotw]. For comparison, we have shown the empirical relation fromSchwenn et al. (2005) for which f (w) = 0.88. For the measured CME half width(w = 38◦), the three relations give f (w) in the range 0.64 to 1.14 (see Table 1). Vrad

obtained from the observed Vexp = 897 kms−1 and f = 1.14 is in the range 1023kms−1 (full ice-cream cone) to 574 kms−1 (flat cone). These values are listed in Table1 along with the deviations from Vrad measured by SA and SB. The deviation is thesmallest for the full ice-cream cone model (7.6% for SA and 3.4% for SB). Thesedeviations are well within the typical errors in height-time measurements (∼ 10%).The flat cone and partial ice-cream cone models deviate the most, up to 84%. TheSchwenn et al. (2005) empirical model deviates by 20 to 34%. Thus the STEREO ob-servations confirm that the full ice-cream cone model fits the observation better thanall other models. A similar result was obtained by Michalek et al. (2009) for limbCMEs observed by SOHO in which both expansion and radial speed were measured.

3. Initial and residual acceleration of CMEs

Acceleration of CMEs is a complex issue because of its spatial and temporal depen-dence during an eruption. At any instance, the acceleration is a vector sum of theacceleration due to Lorentz force, gravity, and the aerodynamic drag (see e.g., Chen& Krall 2003; Vršnak 2008), but different components dominate at different distancesfrom the Sun. For example, the propelling force dominates very close to the Sun. Faraway from the Sun, the gravity and propelling components are weakened consider-ably, making the drag to be dominant. The initial acceleration is positive (mainly dueto the propelling force). The acceleration far away from the Sun is small and could bepositive or negative depending on the CME speed (see e.g., Gopalswamy et al. 2000)and is known as the residual acceleration.

Observationally, it is difficult to measure the CME acceleration close to the sur-

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STEREO and SOHO CME studies 15

Figure 2. Three views of the 2011 February 15 Earth-directed CME from STEREO A (a),SOHO (b), and STEREO B (c). The CME appears as a full halo in the SOHO/LASCO field ofview. STEREO A and STEREO B were located at 87◦ ahead and 94◦ behind Earth, respectively.Height-time measurements made from SOHO/LASCO (d) and STEREO (e) give the expansionand radial speed, respectively. The three types of cone models and the corresponding relationVrad = f (w)Vexp are in (f) along with Schwenn et al. (2005) empirical relation. The point(38◦,1.14) corresponds to the 2011 February 15 CME.

face because coronagraph occulting disk prevents CME measurements up to a certainheight. For example, the acceleration measured in the LASCO C2-C3 FOV is mainlydue to the drag force because CMEs attain a “matured” speed beyond about 3 Rs.Occasionally, the CME leading edge was observed close to the surface from non-coronagraphic observations (X-ray, EUV), which extended the height-time history tothe surface (see e.g., Gopalswamy et al. 1999). LASCO’s innermost telescope C1operated for less than 3 years, and provided CME measurements closer to the surface(1.1–3 Rs). Wood et al. (1999) studied two CMEs by combining EIT, C1, C2, andC3 data and showed that the initial accelerations peaked at 60 and 400 ms−2 and thatthe acceleration ceased before 4 Rs. Gopalswamy & Thompson (2000) used a similarcombination for the 1998 June 11 CME and found that the combined height-time plotcan be fit to a third order polynomial indicating an initial acceleration followed bydeceleration. They found that the CME had an initial acceleration of ∼ 250 ms−2 andthe acceleration ended ∼ 2 hours after the start of the eruption. Zhang et al. (2001)and Zhang & Dere (2006) obtained the initial acceleration of ∼ 50 CMEs by combin-ing the flare rise time and the LASCO CME speed (flare-CME method) and found themean and median values of initial acceleration to be 300 and 200 ms−2, respectively.They also found that the initial acceleration could be occasionally as high as 7 kms−2.Gopalswamy et al. (2012a) obtained the initial acceleration of 483 limb CMEs using

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01:00 02:00 03:00 04:00Start Time (17-May-12 00:50:00)

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Figure 3. Height-time (h-t), speed, and acceleration plots of the 2012 May 17 CME obtainedfrom STEREO COR1, COR2, EUVI, and LASCO C2, C3 data. The line through the speedpoints indicates a slow deceleration. The GOES soft X-ray (SXR) flux and is in arbitrary units.Note that the CME speed peaks around the time of the SXR peak. The acceleration attains amaximum value of 1.77 kms−2.

the flare-CME method and found that CMEs with positive residual acceleration had asmaller initial acceleration (0.75 kms−2) compared to the ones with negative residualacceleration (1.0 kms−2). They also found the initial acceleration to be the highestfor CMEs associated with ground level enhancement (GLE) in solar energetic parti-cle (SEP) events: these CMEs had an average acceleration of 2.3 kms−2 and attainedtheir peak speed before reaching the LASCO/C2 occulting disk. Gopalswamy et al.(2012a) were able to confirm the high initial acceleration of one of the GLE CMEs(2003 November 2 CME at 17:19 UT) using the near-surface observations availablefrom the Mauna Loa Solar Observatory (MLSO), Mark4 K-Coronameter: the MLSOvalue was 2.79 kms−2 compared to 3.82 kms−2 from the flare-CME method.

One of the first results obtained using STEREO’s extended FOV is that the CMEspeed is highly variable within the STEREO/COR1 FOV. Gopalswamy et al. (2009b)found cases (e.g., the 2007 June 3 event) in which the speed attained a high valueof ∼ 925 kms−1 in the COR1 FOV and dropped to ∼ 500 kms−1 by the time theCME reached LASCO/C2 FOV. The flare had a rise time of ∼ 5 min, which givesan initial acceleration of ∼ 3.1 kms−2. Bein et al. (2011) analyzed ∼ 100 CMEsobserved by the STEREO mission and found the initial acceleration to maximize inthe range 0.02 to 6.8 kms−2 consistent with the general range obtained from variousmethods and hence validated those methods. Fig. 3 illustrates the variability in CMEspeed and acceleration for the 2012 May 17 CME (Gopalswamy et al. 2013b), whichhappens to be the only GLE event of solar cycle 24 (to date). The CME was observed

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STEREO and SOHO CME studies 17

Figure 4. Magnetic and plasma signatures of the 2008 June 6 ICME as observed at STEREO B(left) and at L1 (right). The first vertical dashed line corresponds to the shock and the intervalbetween the second and third vertical lines correspond to the ICME.

by LASCO (C2, C3) and STEREO (EUVI, COR1, COR2) so that the height-timehistory is complete. The peak acceleration was ∼ 1.8 kms−2 resulting in a maximumspeed of ∼ 2000 kms−1. The speed and acceleration are consistent with the typicalvalues for GLE events.

The theoretical basis for the high initial acceleration is given in Vršnak (2008),who obtained the upper limit based on the potential field energy available in the sourceregion. Since the potential energy is of the order of the free energy (Mackay et al.1997), one can assume that all the free energy goes into the CME kinetic energy:1/2ρV2 ≤ B2/8π, where ρ is the plasma density and B is the average magnetic fieldin the source region and V is the CME speed. This relation can be written as V ≤ VA,where VA = B/(4πρ)1/2 is the Alfvén speed in the active region corona. If the initialsize of the CME is L, the Alfvén transit time τ = L/VA combined with V gives aninitial acceleration a = V/τ ≤ V2

A/L. For VA = 1000 kms−1 and L = 105 km, one getsa ≤ 10 kms−2. Thus, the near-Sun CME observations from STEREO has helped usunderstand the early kinematic of CMEs.

4. Geometry and flux rope structure of interplanetary CMEs

The basic magnetic structure of a CME is thought to be a flux rope (see e.g., Yeh1995). Observationally, a flux rope is referred to as a magnetic cloud (MC) based on

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the enhanced magnetic field strength, smooth rotation in one of the transverse com-ponents, and low proton temperature (or plasma beta) as defined by Burlaga et al.(1981). If one or more of the signatures is missing, the structure is referred to asnon-MC. The non-MCs may be inherently lacking flux rope (Gosling 1990) or mayhave a flux rope that is not observed due to observational limitations (Gopalswamy2006). By comparing the flare structures at the Sun and the charge state distributionsat 1 AU, Gopalswamy et al. (2013c) found no significant difference between MCs andnon-MCs originating from close to the disk center. This result strongly suggests thatboth MCs and non-MCs form due to a similar process at the Sun: the flare structureand flux rope structure originate from the same eruption process as suggested by the-oretical (Longcope & Beveridge 2007) and observational (Qiu et al. 2007) studies.Furthermore, a flux rope can be fit to CMEs near the Sun irrespective of their inter-planetary manifestation as MCs or non-MCs (Xie et al. 2013). Finally, most of thenon-MCs originating from the disk center undergo deflection due to nearby coronalholes, so they behave like events originating away from the disk center (Mäkelä etal. 2013). Such a deflection would mean that the spacecraft making in situ observa-tions may not be passing through the nose of the flux rope, and hence sees a non-MC.Since STEREO’s in situ observations are made at an angle from the Sun-Earth line,one can directly test the geometrical hypothesis that MCs appear as non-MCs due toobserving angle. Fig. 4 shows in situ observations of an interplanetary CME (ICME)heading towards SB. The ICME has an enhanced magnetic field (B), smooth rota-tion in the east-west direction (By), and low plasma beta. Other signatures such aslow proton temperature (T ), decreasing speed (V) in the ICME interval, a constantnorth-south component (Bz), and a diminished density (n) in the ICME interval arealso consistent with an MC. On the other hand, in situ observations from L1 (OMNIdata) do not show most of the MC signatures. The only clear signatures are the en-hanced magnetic field and the IP shock. At the time of the observations, SB was 25◦

behind Earth. The CME originated from close to the disk center on 2008 June 1 inSB view. Unfortunately, there was a data gap in the EIT data around the onset timeof the CME. However, based on SB information, we expect the source to be aroundE25 in SOHO view. The reason for the event to be barely observed at L1 (OMNIdata) seems to be the high inclination of the magnetic cloud (the axis of the MC is inthe north-south direction). For a low-inclination case, the CME should be observed atlocations separated by 25◦ because the ICME width typically exceeds 60◦. STEREOin situ observations thus provide strong support to the idea that many flux ropes areobserved as non-MCs due to geometrical reasons.

5. Height of shock formation in the solar corona

Type II radio bursts are indicative of shocks formed very close to the Sun. STEREO/

COR1 provided the opportunity to observe the height of shock formation directlyfrom coronagraph images (Gopalswamy et al. 2009b). For limb events, the height ofthe CME leading edge provides an estimate of the height of shock formation. One canalso derive the height of shock formation using EUV images taken at the time of the

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STEREO and SOHO CME studies 19

Figure 5. Radio dynamic spectrum of the 2011 March 7 type II burst which started at a lowfrequency (25 MHz) and had fundamental (F) and harmonic structure (H). (b) STEREO/COR1image with a superposed EUVI image from the Behind spacecraft. The CME was at a height(measured from the Sun center) of 1.93 Rs when the type II burst started at a frequency of 25MHz at 14:25 UT. (c) The distribution of shock formation heights at the time of the type IIburst for the 32 events. (d) The distribution of starting frequency of type II bursts. (d) Thescatter plot showing modest correlation (coefficient R =0.56) between the starting frequencyand the CME height (taken to be the shock height). The empirical fit to the plot shows a powerlaw with an index of 3.64.

type II bursts. In the disk case, the radius of the EUV wave represents the height ofshock formation above the photosphere because, early on, the CME and shock expandspherically. The shock can be represented by a hemispherical structure surroundingthe CME. Gopalswamy et al. (2009b) made use of the COR1 and EUVI data to showthat the CME was at a height < 1.5 Rs when the type II burst started. In this study,the separation between the two STEREO spacecraft was not large (around 25◦).

In a recent study, Gopalswamy et al. (2013a) applied the wave diameter and lead-ing edge methods to determine the shock heights for a set of 32 metric type II burstsfrom Solar Cycle 24. Fig. 5a shows a metric type II burst starting at 14:25 UT on 2011March 7. The type II was due to a west limb CME in SB view as shown in Fig. 5b.Since the SB/COR1 image was taken within seconds of the type II burst onset, theshock formation is accurately known. By choosing events like this, the projectioneffects are minimized: the measurements were made from a view that was roughlyorthogonal to the direction of ejection (this was possible because the STEREO space-

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craft were at large angles with respect to the Sun-Earth line). By choosing imageframes close to the onset times of the type II bursts, the need for extrapolation wasavoided. This study revealed that the CMEs were located in the heliocentric distancerange from 1.20 to 1.93 Rs at the time of type II onset, with mean and median val-ues of 1.43 and 1.39 Rs, respectively (Fig. 5c). This study conclusively finds thatthe shock formation can occur at heights substantially below 1.5 Rs and hence hasimportant implications for the acceleration solar energetic particles (Gopalswamy etal. 2012a; 2013b). In several cases, the observations were made when STEREO andSDO were in quadrature, so it was possible to compare the leading edge and wavediameter methods. The heights from the two methods agreed within a few percent(Gopalswamy et al. 2013a).

In a few cases, the CME height at type II onset was close to 2 Rs and the startingfrequency of the type II bursts was accordingly very low (25–40 MHz, see Fig. 5d).These events confirm that the shock can also form at larger heights. The startingfrequencies of metric type II bursts showed a weak correlation with the measuredCME/shock heights (Fig. 5e). The scatter plot between the starting frequencies andthe CME/shock heights mimics the distribution of plasma frequencies with height.The power law dependence of the plasma frequency with height is consistent with therapid fall off of density low in the corona. The power law index of the frequency falloff with height in the corona (3.64) in Fig. 5e indicates a rapid density fall off (indexof 7.28), which is consistent with the eclipse data and the drift rate spectrum of typeII bursts (Gopalswamy et al. 2009b).

6. Heliospheric magnetic field

White light signatures of shocks have been recently identified as the diffuse featuresurrounding the CME flux rope (Sheeley et al. 2000; Vourlidas et al. 2003; Gopal-swamy et al. 2008; Ontiveros & Vourlidas 2009; Gopalswamy et al. 2009b). For limbevents, the thickness of the diffuse feature is the thickness of the shock sheath, so itrepresents the standoff distance of the shock ahead of the flux rope (Gopalswamy &Yashiro 2011; Ma et al. 2011; Gopalswamy et al. 2012c). The ratio of the standoff

distance (∆R) to the radius of curvature of the flux rope (Rc) is related to the AlfvénicMach number (M) in the upstream of the shock. Assuming the ratio of specific heats(γ), it is possible to determine M because ∆R and Rc can be measured from coron-agraphic observations: ∆R/Rc = 0.81[(γ − 1)M2 + 2]/[(γ + 1)(M2 − 1)] (Russell &Mulligan 2002). Since M = VS /VA, the ratio of the shock speed (VS ) to the Alfvénspeed (VA) in the upstream of the shock, one can measure VS from images and henceget VA. With further determination of the density (n) in the upstream medium by in-verting coronagraphic images (total or polarized brightness images), one can get thecoronal magnetic field. Gopalswamy & Yashiro (2011) measured ∆R, Rc, VS , and nfrom SOHO/LASCO and STEREO/SECCHI images of the 2008 March 25 CME andhence determined the coronal magnetic field. The estimated magnetic field decreasedfrom ∼ 48 mG around 6 Rs to 8 mG at 23 Rs. The radial profile of the magnetic field

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STEREO and SOHO CME studies 21� � � � � � � � � � � � � � � � � � � � � � � �

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Figure 6. A composite plot using the magnetic field strength derived from SDO (Gopalswamyet al. 2012c), SOHO/LASCO and STEREO COR2 (Gopalswamy & Yashiro 2011), COR2 andHI 1 (Poomvises et al. 2012), and Helios in situ measurements. The data point from L1 in situmeasurement is also shown (cross). The power law fit to the Helios data alone and to all thedata are shown on the plot.

can be described by a power law in agreement with other estimates at similar helio-centric distances. These case studies have also been confirmed by a statistical studyinvolving several fast CMEs that clearly showed shock structure in LASCO images(Kim et al. 2012). Note that this is an independent technique to measure the magneticfield in a region of the interplanetary medium that will be probed by the Solar Orbiter,Solar Probe Plus missions in the near future.

Poomvises et al. (2012) extended the determination of the magnetic field strengthto heliocentric distance range up to 120 Rs using data from STEREO/COR2 and HI1instruments. The shock standoff distance of the 2008 April 5 CME and the radiusof curvature of the CME were used for this purpose (see also Maloney & Gallagher2011). The three-dimensional shape of the CME was fit using the Graduated Cylindri-cal Shell model (Thernisien 2011). The radial magnetic field strength was computedfrom the Alfvén speed and density of the ambient medium. The derived magneticfield strength was compared with in situ measurements made by the Helios spacecraftin the heliocentric distance range from 60 to 215 Rs. They found that the radial mag-netic field strength decreases from 28 mG at 6 Rs to 0.17 mG at 120 Rs. In addition,

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22 N. Gopalswamy

they found that the radial profile can be described by a power law that can be extendedto include the in situ measurements at L1. Fig. 6 shows the computed magnetic fieldextending from the lower corona to 1 AU. The radial magnetic field strength in theinterplanetary medium fits well with all the observational data for γ = 5/3. This resultalso suggests that γ = 5/3 may be more appropriate than γ = 4/3.

7. Conclusions

We summarized a number of results obtained using the unique features of STEREOdata: multiple views, extended field of view (inward and outward of the Sun), and theimproved cadence. The main conclusions are:

(i) STEREO confirmed the 3D-bubble structure of CMEs by observing normalCMEs in STEREO view, while the CMEs appeared as halos in Earth view.

(ii) The relation between radial and expansion speed depends on CME width andthe type of ice cream cone as illustrated from multiple views of the same CMEfrom STEREO and SOHO. Full ice-cream cone model represents the observa-tions better than all other models and the empirical model.

(iii) The initial acceleration of CMEs obtained by extrapolation methods have beenconfirmed by direct measurements from STEREO. The initial acceleration canexceed 5 kms−2, and is usually much larger in magnitude than the residualacceleration.

(iv) All CMEs observed in the interplanetary medium are likely to have flux ropestructure. The appearance of CMEs without a flux rope structure may be an ob-servational effect. In situ measurements of the same interplanetary CME fromSTEREO (off of the Sun-Earth line) and L1 confirm this geometrical hypothe-sis.

(v) Type II bursts occur when the CMEs reach a height of ∼ 1.2 Rs, which isroughly the height of shock formation in the corona. Occasionally, shocks canform at a larger height, in which case the starting frequency of the type II burstsis very low.

(vi) The magnetic field in the heliosphere can be measured from coronagraphic ob-servations when CMEs show clear flux rope - shock structure. These measure-ments can be conformed in the near future using Solar Orbiter and Solar ProbePlus data.

Acknowledgements

The author thanks the S. Yashiro, S. Akiyama, H. Xie, and P. Mäkelä for continuedcollaboration. The open data policy of STEREO and SOHO teams is greatly appreci-ated. This work was supported by NASA’s LWS TR&T program.

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STEREO and SOHO CME studies 23

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