STEREO and Wind observations of a fast ICME flank triggering a prolonged geomagnetic storm on 5-7 April 2010

STEREO and Wind observations of a fast ICME flank triggering a prolonged geomagnetic storm on 5-7 April 2010

C. Möstl Space Research Institute, Austrian Academy of Sciences, Schmiedlstr. 6, A-8042, Graz, Austria    M. Temmer Space Research Institute, Austrian Academy of Sciences, Schmiedlstr. 6, A-8042, Graz, Austria    T. Rollett Institute of Physics, University of Graz, Universitätsplatz 5, A-8010, Austria Space Research Institute, Austrian Academy of Sciences, Schmiedlstr. 6, A-8042, Graz, Austria    C. J. Farrugia Space Science Center and Dept. of Physics, University of New Hampshire, Durham, NH 03824, USA    Y. Liu Space Sciences Laboratory, University of California, 7 Gauss Way, Berkeley, CA 94720, USA    A. M. Veronig Institute of Physics, University of Graz, Universitätsplatz 5, A-8010, Austria    M. Leitner Institute for Astro- and Particle Physics, University of Innsbruck, A-6020, Austria    A. B. Galvin Space Science Center and Dept. of Physics, University of New Hampshire, Durham, NH 03824, USA    H. K. Biernat Space Research Institute, Austrian Academy of Sciences, Schmiedlstr. 6, A-8042, Graz, Austria Institute of Physics, University of Graz, Universitätsplatz 5, A-8010, Austria
Abstract

On 5 April 2010 an interplanetary (IP) shock was detected by the Wind spacecraft ahead of Earth, followed by a fast (average speed 650 km/s) IP coronal mass ejection (ICME). During the subsequent moderate geomagnetic storm (minimum = -72 nT, maximum ), communication with the Galaxy 15 satellite was lost. We link images from STEREO/ SECCHI to the near–Earth in situ observations and show that the ICME did not decelerate much between Sun and Earth. The ICME flank was responsible for a long storm growth phase. This type of glancing collision was for the first time directly observed with the STEREO Heliospheric Imagers. The magnetic cloud (MC) inside the ICME cannot be modeled with approaches assuming an invariant direction. These observations confirm the hypotheses that parts of ICMEs classified as (1) long–duration MCs or (2) magnetic–cloud–like (MCL) structures can be a consequence of a spacecraft trajectory through the ICME flank.

\authorrunninghead

MÖSTL ET AL. \titlerunninghead3–5 APRIL 2010 CORONAL MASS EJECTION \authoraddrC. Möstl, Space Research Institute, Austrian Academy of Sciences, Schmiedlstr. 6, Graz, A-8042, Austria. (christian.moestl@oeaw.ac.at)

\setkeys

Gindraft=false

{article}

1 Introduction

A major obstacle to making progress in our understanding of the characteristics of coronal mass ejections (CME) in the interplanetary medium (ICMEs) has always been the fact that single spacecraft in situ observations enormously undersample an ICME’s global structure. While the observations of the interplanetary (IP) magnetic field, plasma parameters and composition have proven to be extremely useful in the past and lead to a paradigm that a subset of ICMEs are huge magnetic flux ropes bent on a global scale (Burlaga et al., 1981; Lepping et al., 1990), much is still unknown. Even the basic question as to whether all ICMEs include flux ropes or whether there are ICMEs that lack flux ropes lacks a definitive answer (e.g. Riley et al., 2006). This is linked to the fact that it is very hard to interpret the signatures of ICMEs observed by a single spacecraft, which are usually categorized into magnetic clouds (MCs), magnetic–cloud–like (MCL) structures or ejecta (e.g. Lepping et al., 2006), depending on the “clarity” of the signature. Often it is totally unclear where the spacecraft intercepts the ICME with respect to its cross section and/or its global shape. The NASA STEREO mission (Kaiser et al., 2008), consisting of two spacecraft increasingly separating themselves from the Earth in the ecliptic, was launched in 2006 to tackle this problem from two angles: by providing multi–spacecraft in situ observations (e.g. Kilpua et al., 2009; Möstl et al., 2009a), and by imaging ICMEs in white light along the entire Sun–Earth line with the Heliospheric Imager (HI) instrument (Eyles et al., 2009). Several authors have discussed ICMEs sweeping over an in situ observing spacecraft in the HI images (e.g. Davis et al., 2009; Möstl et al., 2009b; Liu et al., 2010) and found in general good correspondences between CME/ICME directions, orientations and arrival times. But all of the events discussed so far were slow ICMEs, typical of the recent solar minimum. With solar activity now on the rise, the opportunity to study fast (flare–associated) and thus more geo–effective ICME events comes into focus.

In this Letter, we report on the first fast ICME ( km/s) which was observed by STEREO/HI for the full Sun–Earth line and which was associated with a MC and a geomagnetic storm at Earth. The observations for the first time unambiguously show that the ICME flank produced signatures of a long–duration MC, which acted as the interplanetary driver for a three–day geomagnetic storm, with a maximum and a minimum  nT. Though moderate, the storm was nonetheless responsible for a communication failure which led to the loss of the Galaxy 15 satellite 111Denig, W. and Green J. et al., Space Weather Conditions at the Time of the Galaxy 15 Spacecraft Anomaly, NOAA, Boulder, CO, 1 June 2010. . We discuss the interplanetary propagation of the ICME and the characteristics of the embedded MC near Earth.

2 Interplanetary propagation

Figure 1: (a) Overview of the observing geometry and spacecraft positions, looking down from ecliptic north. Blue sphere: COR2 field of view (, see panel (b)). Green circles: Thomson surfaces of maximized intensity for STEREO–A/B. Indicated are CME directions from Fixed– fitting for the STEREO–A CME track (Fig. 2b, FP, red), and the stereoscopic techniques of Liu triangulation (LT, black) and forward modeling (FM, blue). (b) FM using COR2A (top) and COR2B (bottom) images of the CME at .

Figure 1a gives an overview of the spacecraft positions and the observing geometry on 5 April, 2010. STEREO–Ahead(Behind) was separated to Earth by in the ecliptic (the separation in latitude is negligible). The HI1 and HI2 cameras onboard STEREO–A/B (field of views indicated) image photospheric white–light scattered off solar wind electrons. The resultant observed intensity is maximized at the Thomson surface (green circles in Fig. 1a), a sphere with the Sun–observer distance as diameter and centered halfway between the Sun and the observer.

The Thernisien et al. (2009) forward modeling (FM) method, assuming a “croissant–shaped” CME, was applied successfully to COR2A and COR2B images. The STEREO/SECCHI COR2 coronagraph covers the corona from 2–15 , with the field of view indicated as a blue sphere in Fig. 1a. An example is shown in Figure 1b. The resulting direction with respect to the Sun–Earth line is S27 () and W0 () (i.e. south of the ecliptic and earthward), so the ICME propagated radially from the site of the associated B7.4 flare at S25W03 (GOES 1–8 Å  flux peaked on 3 Apr, 09:54 UT).

Figure 2 focuses on STEREO–A HI observations from  AU and Wind at 1 AU. The images were reduced according to Davies et al. (2009) and are presented as running differences. The ICME was also observed by HI on STEREO–B, but the morphology in HI1B was very similar to HI1A and the ICME signal in HI2B was very noisy because of the milky way in the background. Figure 2a shows the CME morphology observed by HI1/2A. The front density enhancement is the sheath region behind the shock later observed in situ, extending much wider in latitude than the driver, especially in HI2A. Two other features are indicated, one being the southward directed core of the CME and the other, around the ecliptic, a density loop, which was not observed by Wind later, but could be related to the ICME “back” region (see below). We encourage the reader to look at a combined movie of the HIA images and the Wind density available online, where it is clearly seen that the CME apex was southward directed and that its northern flank passed over Earth.

Figure 2b shows a time–elongation Jplot of the ecliptic plane (e.g. Davies et al., 2009) with the ICME track reaching up to the Earth as well as the proton density observed by Wind. It is seen that the ICME leading edge (LE) corresponded to the density enhancement observed by Wind, although the the LE was about 4 hours too early at the elongation of Wind when compared to the shock arrival time 5 Apr, 07:58 UT. This seems to be a geometric effect of the ICME front shape as the observer does not look exactly along LE when it hit Wind. Figure 2c shows a time–distance and a time–velocity plot converted from the elongation extracted along the LE in the Jplot using the methods of Fixed- (Kahler and Webb, 2007), with direction with respect to Earth (solar west is positive) and Harmonic Mean (Lugaz et al., 2009), with . These directions were chosen so that is consistent with the shock arrival time at Wind. The error bars were estimated from tracking the LE for 10 times manually in the Jplot.

The profile was derived by using a spline fit for , and shows not much deceleration for either method, from about  km/s at 0.1 AU to  km/s near Earth. The velocity closer to the Sun is consistent with the maximum radial speed  km/s obtained with the stereoscopic FM method, and the value at 1 AU is confirmed by the Wind in situ velocity (see below).

Figure 2: STEREO–A HI and Wind observations: (a) CME time evolution in HI1A (left 2 images) and HI2A (right 2 images). ICME features and the position of the Earth (E) and STEREO-B (B) are indicated. (b) Proton density measured by Wind and a HI1A / HI2A Jplot extracted along the ecliptic plane. Increased densities in the ICME sheath are delimited by vertical lines. (c) The time–distance (top) and time–velocity profiles of the CME up to 1 AU, using the Fixed– (red) and Harmonic mean (blue) conversion methods, compared to Wind measurements of the shock arrival time and in situ plasma bulk velocity in the sheath.

3 Wind magnetic cloud observations

Figure 3 shows the in situ observations by Wind SWE (Ogilvie et al., 1995) and MFI (Lepping et al., 1995). The first solid line from left is the shock arrival on 3 April 2010, 07:58 UT. The second and third solid lines indicate the magnetic cloud interval, from 5 Apr, 12:05 UT, to 6 Apr, 13:20 UT. The MC fulfills the Burlaga et al. (1981) criteria of low solar wind proton temperature, low plasma- and a smoothly rotating and higher–than–average total magnetic field ( nT), but it cannot be fitted using the force–free model (Lepping et al., 1990) or reconstructed with the Grad–Shafranov technique (Hu and Sonnerup, 2002). Quantitatively comparing the force–free model fit to the observations results in , a parameter defined by Lynch et al. (2003), which indicates that no good fits were found by using various intervals. Thus it is, strictly speaking, classified as a MCL (Lepping et al., 2006). The MCL can be divided into two parts: (1) a region where B rotates and declines, with a size along the spacecraft trajectory of 0.24 AU, and (2) a “back region” (starting 6 Apr, 02:00 UT) where the is constant and B does not rotate (0.16 AU). These are the first combined observations of a ICME flank in heliospheric images and its in situ magnetic field and demonstrate that the ICME magnetic field at the flank is not consistent here with the classic picture of magnetic clouds consisting of clearly helical magnetic field lines. The asymmetry in , peaking at the beginning of the MCL passage, is usually attributed to its expansion (which is evident in the velocity in Fig. 3), but this would only lead to a shift in towards the front (Farrugia et al., 1995). We thus think that these particular signatures of B reflect 3D aspects of the MCL, such as strong curvature or a different internal structure of B at the ICME flank.

We also estimated the MCL axis orientation with minimum variance analysis (MVA) to (in GSE xyz, pointing northward and eastward) and the shock normal orientation using the co-planarity theorem yielding . These are perpendicular to one another to within an angle from 84 to 110 degrees for various intervals used for both the shock and MVA analyses. This means that the spacecraft crossed the MCL at the flank where the ejecta was still driving the shock.

In Fig. 3, the development of the and indices is shown. Looking at the profile of , it is clear that a strong (minimum =  nT) and short interval of negative in the sheath coincided with the storm commencement. In the ICME back region, too, it is the negative which is responsible for prolonging the storm growth phase. In between these two regions, when  nT, it is the large, negative which accounts for the continued ring current intensity.

Figure 3: Magnetic field and plasma data (Wind). From top to bottom: magnetic field magnitude and components in GSE coordinates (X pointing towards the Sun, Y points to solar east and Z is normal to the ecliptic), proton bulk velocity, proton number density, proton temperature, plasma , indices: (blue bars, every 3 hours) and (green line, hourly). The first solid line from left is the shock arrival. Second and third solid lines indicate the MC interval. A black dashed line inside the MC marks the begin of the “back” region (see text). The arrival time (red dashed line) and velocity (red horizontal line) from the Fixed– fitting method are also shown. The extent of the horizontal line is the error in the arrival time.

As a consistency check, we also examined the fitting method for the CME LE elongation profile (Rouillard et al., 2008) based on the Fixed- conversion formula, which assumes a point–like CME, using the complete track. The red dashed line in Fig. 3 is the calculated arrival time on 5 Apr, 06:26 UT +/- 4h (Wind shock arrival 07:58 UT). The horizontal red bar gives the fitting velocity ( km/s) and its extent indicates the arrival time error. Also the CME direction degrees (red straight line in Fig. 1) is consistent with the flare source region longitude and the FM results (blue short line), as well as with the CME trajectory (black line with error bars) obtained by the triangulation technique described in Liu et al. (2010) using both HIA/B Jplots (not shown).

4 Summary and Conclusions

Our main findings are:

  1. We reported on the first STEREO observations of a fast CME/ICME event with an associated geo-effective MC observed completely from the Sun to 1 AU.

  2. The flank part of the ICME in HI only weakly decelerated from roughly 1000 km/s to 800 km/s between the Sun and 1 AU, with the HI velocity values constrained and confirmed by the FM method close to the Sun and the Wind in situ velocity at 1 AU.

  3. We combined remote HI images by STEREO-A/B at about 70 degrees separation to Earth with the Wind plasma and magnetic field in situ observations. This shows that intervals in the front part of the sheath and particular in a long “back region” of the MCL at the ICMEs northern flank drove the long growth phase of the storm.

  4. The event demonstrates that long–duration magnetic clouds and MCLs can be a consequence of observations through the ICME flank, as assumed by Marubashi and Lepping (2007).

The observations emphasize the selection effect imposed by a particular trajectory through an ICME. They shed light on the problem that some MCs which fulfill the Burlaga et al. (1981) definition have profiles which cannot be modeled using standard approaches such as force-free modeling (Lepping et al., 1990) and Grad–Shafranov reconstruction (Hu and Sonnerup, 2002), which treat the MC as being of local cylindrical or invariant symmetry. We speculate that in such cases a model is needed which takes into account local curvature (e.g. the one by Marubashi and Lepping, 2007). We note that the characteristics of this MCL can be taken as representative of other observations where it is unknown where the spacecraft intercepts the ICME.

Another interesting fact is that the MCL profile is very reminiscent of the events discussed by, e.g., Dasso et al. (2007) who interpreted long “back” regions with non–rotating magnetic fields behind MCs as caused by reconnection of the MC with the interplanetary magnetic field. From the observations presented here it becomes clear that another plausible explanation of these non-rotating, constant fields is a purely geometrical effect: when the spacecraft intercepts a ICME flank where the field lines are no longer helical.

Acknowledgements.
C.M., M.T., T.R., A.V. and H.K.B. acknowledge the Austrian Science Fund (FWF):[P20145-N16]. We thank Janet Luhmann and Claire Foullon for useful discussions. Work at UNH is supported by NASA grants NNX08AD11G, NNX10AQ29G and NASA STEREO grant to UNH. Work at UCB was supported from STEREO grant NAS5-03131. We also acknowledge the use of Wind data provided by the magnetometer and the solar wind experiment teams at GSFC, and thank the STEREO/ SECCHI teams for their open data policy. We also thank the centers for geomagnetism in Kyoto and Potsdam.

References

  • Burlaga et al. (1981) Burlaga, L., E. Sittler, F. Mariani, and R. Schwenn (1981), Magnetic loop behind an interplanetary shock - Voyager, Helios, and IMP 8 observations, J. Geophys. Res., 86, 6673–6684.
  • Dasso et al. (2007) Dasso, S., M. S. Nakwacki, P. Démoulin, and C. H. Mandrini (2007), Progressive Transformation of a Flux Rope to an ICME. Comparative Analysis Using the Direct and Fitted Expansion Methods, Sol. Phys., 244, 115–137, doi:10.1007/s11207-007-9034-2.
  • Davies et al. (2009) Davies, J. A., et al. (2009), A synoptic view of solar transient evolution in the inner heliosphere using the Heliospheric Imagers on STEREO, Geophys. Res. Lett., 36, 2102, doi:10.1029/2008GL036182.
  • Davis et al. (2009) Davis, C. J., J. A. Davies, M. Lockwood, A. P. Rouillard, C. J. Eyles, and R. A. Harrison (2009), Stereoscopic imaging of an Earth-impacting solar coronal mass ejection: A major milestone for the STEREO mission, Geophys. Res. Lett., 36, 8102, doi:10.1029/2009GL038021.
  • Eyles et al. (2009) Eyles, C. J., et al. (2009), The Heliospheric Imagers Onboard the STEREO Mission, Sol. Phys., 254, 387–445, doi:10.1007/s11207-008-9299-0.
  • Farrugia et al. (1995) Farrugia, C. J., V. A. Osherovich, and L. F. Burlaga (1995), Magnetic flux rope versus the spheromak as models for interplanetary magnetic clouds, J. Geophys. Res., 100, 12,293.
  • Hu and Sonnerup (2002) Hu, Q., and B. U. Ö. Sonnerup (2002), Reconstruction of magnetic clouds in the solar wind: Orientations and configurations, Journal of Geophysical Research (Space Physics), 107, 10–1, doi:10.1029/2001JA000293.
  • Kahler and Webb (2007) Kahler, S. W., and D. F. Webb (2007), V arc interplanetary coronal mass ejections observed with the Solar Mass Ejection Imager, Journal of Geophysical Research (Space Physics), 112, 9103, doi:10.1029/2007JA012358.
  • Kaiser et al. (2008) Kaiser, M. L., T. A. Kucera, J. M. Davila, O. C. St. Cyr, M. Guhathakurta, and E. Christian (2008), The STEREO Mission: An Introduction, Space Science Reviews, 136, 5–16, doi:10.1007/s11214-007-9277-0.
  • Kilpua et al. (2009) Kilpua, E. K. J., et al. (2009), Multispacecraft Observations of Magnetic Clouds and Their Solar Origins between 19 and 23 May 2007, Sol. Phys., 254, 325–344, doi:10.1007/s11207-008-9300-y.
  • Lepping et al. (1990) Lepping, R. P., L. F. Burlaga, and J. A. Jones (1990), Magnetic field structure of interplanetary magnetic clouds at 1 AU, J. Geophys. Res., 95, 11,957–11,965.
  • Lepping et al. (2006) Lepping, R. P., D. B. Berdichevsky, C. Wu, A. Szabo, T. Narock, F. Mariani, A. J. Lazarus, and A. J. Quivers (2006), A summary of WIND magnetic clouds for years 1995-2003: model-fitted parameters, associated errors and classifications, Annales Geophysicae, 24, 215–245.
  • Lepping et al. (1995) Lepping, R. P., et al. (1995), The Wind Magnetic Field Investigation, Space Science Reviews, 71, 207–229.
  • Liu et al. (2010) Liu, Y., J. A. Davies, J. G. Luhmann, A. Vourlidas, S. D. Bale, and R. P. Lin (2010), Geometric Triangulation of Imaging Observations to Track Coronal Mass Ejections Continuously Out to 1 AU, ApJ, 710, L82–L87, doi:10.1088/2041-8205/710/1/L82.
  • Lugaz et al. (2009) Lugaz, N., A. Vourlidas, and I. I. Roussev (2009), Deriving the radial distances of wide coronal mass ejections from elongation measurements in the heliosphere - application to CME-CME interaction, Annales Geophysicae, 27, 3479–3488.
  • Lynch et al. (2003) Lynch, B. J., T. H. Zurbuchen, L. A. Fisk, and S. K. Antiochos (2003), Internal structure of magnetic clouds: Plasma and composition, Journal of Geophysical Research (Space Physics), 108, 1239, doi:10.1029/2002JA009591.
  • Marubashi and Lepping (2007) Marubashi, K., and R. P. Lepping (2007), Long-duration magnetic clouds: a comparison of analyses using torus- and cylinder-shaped flux rope models, Annales Geophysicae, 25, 2453–2477.
  • Möstl et al. (2009a) Möstl, C., C. J. Farrugia, H. K. Biernat, M. Leitner, E. K. J. Kilpua, A. B. Galvin, and J. G. Luhmann (2009a), Optimized Grad-Shafranov Reconstruction of a Magnetic Cloud Using STEREO- Wind Observations, Sol. Phys., 256, 427–441, doi:10.1007/s11207-009-9360-7.
  • Möstl et al. (2009b) Möstl, C., C. J. Farrugia, M. Temmer, C. Miklenic, A. M. Veronig, A. B. Galvin, M. Leitner, and H. K. Biernat (2009b), Linking Remote Imagery of a Coronal Mass Ejection to Its In Situ Signatures at 1 AU, ApJ, 705, L180–L185, doi:10.1088/0004-637X/705/2/L180.
  • Ogilvie et al. (1995) Ogilvie, K. W., et al. (1995), SWE, A Comprehensive Plasma Instrument for the Wind Spacecraft, Space Science Reviews, 71, 55–77.
  • Riley et al. (2006) Riley, P., C. Schatzman, H. V. Cane, I. G. Richardson, and N. Gopalswamy (2006), On the Rates of Coronal Mass Ejections: Remote Solar and In Situ Observations, ApJ, 647, 648–653, doi:10.1086/505383.
  • Rouillard et al. (2008) Rouillard, A. P., et al. (2008), First imaging of corotating interaction regions using the STEREO spacecraft, Geophys. Res. Lett., 35, 10,110, doi:10.1029/2008GL033767.
  • Thernisien et al. (2009) Thernisien, A., A. Vourlidas, and R. A. Howard (2009), Forward Modeling of Coronal Mass Ejections Using STEREO/SECCHI Data, Sol. Phys., 256, 111–130, doi:10.1007/s11207-009-9346-5.
Comments 0
Request Comment
You are adding the first comment!
How to quickly get a good reply:
  • Give credit where it’s due by listing out the positive aspects of a paper before getting into which changes should be made.
  • Be specific in your critique, and provide supporting evidence with appropriate references to substantiate general statements.
  • Your comment should inspire ideas to flow and help the author improves the paper.

The better we are at sharing our knowledge with each other, the faster we move forward.
""
The feedback must be of minimum 40 characters and the title a minimum of 5 characters
   
Add comment
Cancel
Loading ...
121548
This is a comment super asjknd jkasnjk adsnkj
Upvote
Downvote
""
The feedback must be of minumum 40 characters
The feedback must be of minumum 40 characters
Submit
Cancel

You are asking your first question!
How to quickly get a good answer:
  • Keep your question short and to the point
  • Check for grammar or spelling errors.
  • Phrase it like a question
Test
Test description