Space weather refers to dynamic conditions on the Sun and in the space environment of the Earth, which are often driven by solar eruptions and their subsequent interplanetary disturbances. It has been unclear how an extreme space weather storm forms and how severe it can be. Here we report and investigate an extreme event with multi-point remote-sensing and in situ observations. The formation of the extreme storm showed striking novel features. We suggest that the in-transit interaction between two closely launched coronal mass ejections resulted in the extreme enhancement of the ejecta magnetic field observed near 1 AU at STEREO A. The fast transit to STEREO A (in only 18.6 h), or the unusually weak deceleration of the event, was caused by the preconditioning of the upstream solar wind by an earlier solar eruption. These results provide a new view crucial to solar physics and space weather as to how an extreme space weather event can arise from a combination of solar eruptions.
While coronal mass ejections (CMEs), large-scale expulsions of plasma and magnetic field from the solar corona, have been recognized as drivers of major space weather effects, some fundamental questions for solar physics and space weather have not been addressed. Specifically, how does an extreme space weather storm form and evolve, and how severe can it be especially when it reaches the Earth?
An extreme space weather storm is termed a low-probability, high-consequence event, otherwise called a solar superstorm1,2. The largest known example of extreme space weather before the space era is the 1859 Carrington event3. It produced a geomagnetic storm, whose minimum Dst is estimated4 to be approximately −850 nT. The Dst index is a measure of the severity of geomagnetic storms (the more negative the more intense). The most severe geomagnetic storm of the space age has a minimum Dst of −548 nT and was caused by the 13 March 1989 solar wind disturbance5, which led to the collapse of Canada’s Hydro-Québec power grid and a resulting loss of electricity to six million people for up to 9 h. Therefore, understanding extreme space weather is also vital to the modern society and its technological infrastructures.
A statistical analysis6 suggests that CME speeds near the Sun range from several tens to about 3,000 km s−1. In particular, the limit of 3,000 km s−1 is argued to indicate an upper bound to the maximum energy available to a CME from solar active regions7. Most CMEs, however, end up with speeds and magnetic fields comparable to those of the ambient solar wind when they reach the Earth, that is, about 450 km s−1 and 10 nT, respectively8,9. This implies that, while the active region may decide how energetic a CME can be near the Sun7, the subsequent evolution in interplanetary space is also crucial in determining its severity at the Earth. How decisive the interplanetary evolution is remains unclear.
A new view of how extreme space weather can be created by CME–CME interactions in interplanetary space is discovered from the 23 July 2012 event, which had a maximum speed of 3,050±260 km s−1 near the Sun. This event, with complete modern remote-sensing and in situ observations from multiple vantage points, provides an unprecedented opportunity to study the cause (and perhaps consequences as well) of extreme space weather. We illustrate how successive CMEs can be enhanced into a superstorm as they interact en route from the Sun to 1 AU. Note that, while there are many parameters that could be used to measure the extreme or severity of a solar storm5,10,11, here we focus on the solar wind transient speed (v) and magnetic field (B) at a distance of ~1 AU. This is because their cross product, the dawn-dusk electric field (see Methods), controls the rate of the solar wind energy coupling to the terrestrial magnetosphere12. The CME–CME interactions studied here produced an extremely high solar wind speed of 2,246±110 km s−1 and an unusually strong ejecta magnetic field of 109±1 nT observed near 1 AU at STEREO A. This record solar wind speed and magnetic field would have generated the most severe geomagnetic storm since the beginning of the space era, if the event had hit the Earth. The extreme space weather generation scenario is similar to the case of a ‘perfect storm’, a phrase which was initially coined for the October 1991 Atlantic storm but now describes any event where a rare combination of circumstances will aggravate a situation drastically.
Multi-point imaging observations
Figure 1 shows the positions of three widely separated spacecraft in the ecliptic plane, including the Solar and Heliospheric Observatory (SOHO)13 upstream of the Earth and the Solar Terrestrial Relations Observatory (STEREO)14. STEREO comprises two spacecraft with one preceding the Earth (STEREO A) and the other trailing behind (STEREO B). During the time of the solar eruptions on 23 July 2012, STEREO A and B were 121.3° west and 114.8° east of the Earth with a distance of 0.96 AU and 1.02 AU from the Sun, respectively. The event originated from sunspot group NOAA 11520 (S15°W133°), so the source location on the Sun was 43° behind the west limb from the point of view of the Earth, whereas about 12° west of the central meridian as viewed from STEREO A and about 22° behind the east limb for STEREO B. Obviously, STEREO A gives the best observations of the activity on the solar disk, while STEREO B and Earth (SOHO) provide the best views of the associated CMEs. In particular, STEREO B provides a view of the low coronal activity with minimized projection effects.
The event started with two consecutive prominence eruptions separated by about 10–15 min, as shown in Fig. 2a–c (see also Supplementary Movie 1). At 02:27 UT (Fig. 2b), the first erupting prominence (E1) was not visible any more, but a CME (CME1) appeared in COR1 of STEREO B. The second erupting prominence (E2) was still rising and produced a bulging of the coronal structure just south of CME1, which was later recognized as the south edge of the second CME (CME2). The north edge of CME2 was not clear and likely overlapped with CME1. The erupting prominence E2 (Fig. 2c), however, was even visible in the field of view of COR1 and overlapped with a structure with enhanced brightness, so the erupting prominence E2 at 02:37 UT probably marked the core of CME2. At about the same time (02:36 UT), the leading edge of CME1 had already propagated beyond the field of view of COR1 (Fig. 2c). The second eruption appeared stronger than the first one. In COR2 of STEREO B (Fig. 2d,e; Supplementary Movie 2), definite twin-CME signatures were lost presumably due to the CME–CME interaction, although a concave-outward structure may give an impression of two CMEs interweaved together. A shock signature, indicated by a weak edge ahead of the CME front15, was already developed. COR2 aboard STEREO A (Fig. 2g,h; Supplementary Movie 3) first saw material largely west of the Sun at 02:54 UT, but later the event was almost east-west symmetric, which may indicate a change in the longitudinal propagation direction. SOHO gave another side view of the event (Fig. 2f,i) but did not see clear twin-CME signatures. This is probably due to the low time resolution of LASCO (12 min) and a missing image at 03:00 UT for LASCO/C2. The two CMEs occurred so close that one could also argue for a complex single event composed of two eruptions.
Figure 3 shows the time-elongation maps, which are produced by stacking the running difference images within a slit along the ecliptic plane (here we take a position angle of 90° measured counterclockwise from the solar north for STEREO B while clockwise for SOHO)16,17,18. The time-elongation map from COR1 of STEREO B shows two adjacent tracks (Fig. 3b), which agrees with the observations of two closely launched CMEs (Fig. 2a–c; Supplementary Movie 1). These two tracks seem to merge in the map from COR2 of STEREO B. The time-elongation map from LASCO/C2 also appears to have two adjacent tracks around 03:00 UT (Fig. 3a), but, because of the low time resolution and a missing image at 03:00 UT, the correspondence between SOHO and STEREO B cannot be established for the second track.
CME kinematics and flare EUV flux
We determine the kinematics of the CME leading front with a triangulation technique18,19. This technique has no free parameters and has had success in tracking interplanetary propagation of various CMEs20,21,22,23,24,25,26. STEREO B and SOHO provide the best elongation measurements owing to their vantage points, as shown in Fig. 3. Elongation angles are extracted from the leading track in the time-elongation maps, as there is no ambiguity in identifying the correspondence between SOHO and STEREO B for the leading track. The elongation angles are then used as input to the triangulation technique. Uncertainties in the elongation measurements can be used to evaluate the errors in the propagation direction, radial distance and speed of the CME front18,19.
The resulting kinematics in the ecliptic plane are displayed in Fig. 4. The propagation direction is converted to an angle with respect to the Sun-STEREO A line. If the angle is positive (negative), the CME front would be propagating west (east) of the Sun-STEREO A line. The propagation angle started from about the solar source longitude and then showed a transition towards the Sun-STEREO A line. The change in the propagation direction occurred at 02:42–03:05 UT when the CME front reached about 6–11 solar radii. This is consistent with the CME images seen by COR2 of STEREO A (Fig. 2g,h). The change in the propagation angle had a good timing with, and was thus probably caused by, the CME–CME interaction during their merging. The amount of the longitudinal deflection is about 10°, similar to a previous CME–CME interaction case27. The speed of the CME leading edge first increased to about 3,050 km s−1 around 03:14 UT at a distance of about 13 solar radii and then decreased to about 2,700 km s−1.
Measurements of X-ray emissions from the associated flare are not available, so we use the full-disk EUV flux at 195 Å observed by STEREO A as a proxy (Fig. 4c). The EUV flux at 195 Å is proved to be a good tracer of the X-ray emission in the 1–8 Å band; the magnitude of the flare associated with the 23 July 2012 event is at most X2.5 estimated from the relationship between the EUV and X-ray fluxes28. The flare is not particularly intense compared with the Carrington (>X10), 28 October 2003 (>X17) and 4 November 2003 (X28) flares5, which is surprising given how extreme the solar wind disturbance was. This raises an intriguing and important question of how the event became extreme in interplanetary space. The EUV flux shows two peaks with a time separation of about 15 min. This is consistent with the two consecutive eruptions seen in the EUV images at 304 Å from STEREO B (Fig. 2a–c). The CME peak speed was about 30 min after the maximum EUV flux, which may suggest further acceleration post the flare maximum22.
In situ measurements of the extreme storm
Figure 5 shows the in situ measurements from the PLASTIC and IMPACT instruments aboard STEREO A at 0.96 AU. A forward shock passed STEREO A at 20:55 UT on 23 July, with a transit time of only 18.6 h (if we take 02:20 UT as the CME launch time). Two interplanetary CMEs (ICMEs), in situ counterpart of CMEs, can be identified from the magnetic field measurements behind the shock. Across the shock and ICMEs, the proton density and temperature measurements are largely missing here because the conditions exceeded the nominal detector ranges. We use the density of electrons with energies above 45 eV (multiplied by a factor of 5) as a proxy of the plasma density. It matches the proton density well when the proton data are available during the time interval. The solar wind speed jumps from about 900 to 2,246 km s−1 across the shock, which is a remarkably high increase. Both the post-shock peak speed (2,246 km s−1) and the peak magnetic field strength (109 nT) in the early part of the ejecta are among the few largest on record ever measured near 1 AU. Extremely fast solar wind with a speed of ~2,000 km s−1 was measured near 1 AU on two occasions previously, the 4–5 August 1972 and 29–30 October 2003 events29,30. The peak magnetic field associated with the two previous events is about 110 and 68 nT, respectively, which occurred only briefly in the sheath region between the shock and ejecta. The present case, however, has the maximum magnetic field taking place in the first ICME (ICME1), and the ejecta magnetic fields larger than 60 nT lasted for over 6 h.
The magnetic field components are given in RTN coordinates, where R points from the Sun to the spacecraft, T is parallel to the solar equatorial plane and along the planet motion direction and N completes the right-handed system. The two ICMEs seem to have quite different magnetic configurations. Reconstruction assuming a flux-rope geometry31,32 gives a right-handed structure for both of the ICMEs. Their axis orientations, however, are very oblique with respect to each other: an elevation angle of about 69° and azimuthal angle of about 226° (in RTN coordinates) for ICME1, and an elevation angle of about −44° and azimuthal angle of about 186° for ICME2. These axis orientations should be considered as rough estimates, as we do not have good density and temperature measurements and the magnetic field structures of the two ICMEs are irregular.
The magnetic field has a sustained southward component (negative BN), which was larger than 20 nT for more than 5 h (with a maximum value of 52 nT inside ICME2). The extremely high solar wind speed combined with the prolonged strong southward field component would produce an extremely severe geomagnetic storm if the event hit the Earth. We evalute the Dst index using two empirical formulae33,34, based on the solar wind measurements (see Methods). The resulting Dst profiles show a classic geomagnetic storm sequence: a sudden commencement caused by the shock, a main phase and then a recovery phase. The difference between the two Dst profiles is owing to different assumptions on the decay of the terrestrial ring current in the two formulae (see Methods). ICME1 does not produce negative Dst values because of its largely northward magnetic fields. The minimum Dst value is −1,150 and −600 nT, respectively. This is more intense than the most severe geomagnetic storm of the space era caused by the March 1989 event5. The modelled minimum Dst is comparable to that of the 1859 Carrington event4, the largest known solar disturbance before the space age. These results are consistent with previous estimates or speculations35,36,37.
The average transit speed is about 2,150 km s−1, obtained by dividing the distance of STEREO A (0.96 AU) by 18.6 h. This is comparable to the peak solar wind speed at STEREO A, which implies that the event was not slowed down much by the ambient medium. Comparing the CME speed near the Sun (3,050 km s−1) with the peak solar wind speed at STEREO A gives a slowdown of only about 800 km s−1. Since CME deceleration is due to interactions with the ambient solar wind, an initially faster CME will have a stronger deceleration20,38. The minimal slowdown of the present case as well as the extremely strong magnetic field is surprising and raises a question of how the speed and internal magnetic field of the event were maintained or achieved during transit from the Sun to 1 AU.
Generation of the extreme speed and magnetic field
The cause of the minimal slowdown of the 23 July 2012 event is of particular interest. Figure 6 shows an ICME (ICME0) preceding the 23–24 July event. Two forward shocks are also observed ahead of ICME0, which may indicate a series of eruptions on the Sun before the 23 July event. ICME0 was probably produced by a CME launched around 05:30 UT on 19 July with a peak speed of about 1,600 km s−1 from the same active region (AR 11520) as the 23 July event. The region trailing ICME0 has a density as low as 1 cm−3. This low density was likely caused by, first, removal of some of the solar wind plasma by the series of preceding eruptions including ICME0, and, second, further rarefaction by the fast motion of ICME0. The magnetic field in the same region predominantly lies along the radial direction from the Sun, presumably due to stretching of the post-event field by ICME0. These observations indicate that the 23 July complex event was moving through a density depletion region with radial magnetic fields. The significantly reduced solar wind drag and field line tension force can explain the marginal slowdown of the 23 July event.
Combination of the imaging observations with in situ measurements suggests that the mechanism of creating the extremely strong magnetic field is CME–CME interaction. The time interval of ICME1 is very short (Fig. 5), probably owing to compression by ICME2 from behind. This compression started from the nascent stage of the CMEs (Fig. 2) and continued all the way to large distances as revealed by a speed drop in the interaction interface between the two ICMEs (Fig. 5b). A possible scenario is that a shock driven by CME2 was first overtaking CME1 from behind before the direct compression by CME2 occurred. The shock would strengthen the magnetic field inside CME1 as well when it was propagating through and compressing CME1 (refs 21, 39, 40). The magnetic field inside CME2 would also appear enhanced because the expansion of CME2 was inhibited by the CME–CME interaction.
Information from solar wind suprathermal electrons supports the picture of CME–CME interaction, as shown in Fig. 7. The pitch angle (PA; the angle between the electron motion direction and the magnetic field) distribution of the electrons and their heat flux (thermal energy flux carried by the electrons) parallel to the magnetic field trace the magnetic field topology very well: whenever BR switches between negative (sunward) and positive (anti-sunward), the PAs flip between 180° and 0° and the parallel heat flux changes between negative and positive correspondingly. This indicates that the electron beams always move away from the Sun along the magnetic field. Bidirectional streaming electrons (electrons that exhibit peak flux both parallel and anti-parallel to the magnetic field), a typical signature of ICMEs, are not observed during the time period of Fig. 7. The PA distribution becomes irregular in the region between the two ICMEs, confirming its identification of the interaction interface. At 01:51 UT on 24 July, the magnetic field components and the parallel heat flux showed an abrupt change. This is probably the heliospheric current sheet entrained in the CME–CME interaction region. The largest heat flux is seen in the sheath region between the shock and ejecta, presumably owing to shock compression. The heat flux is also enhanced in ICME1 and the interaction interface but decreases into ICME2, which is consistent with the situation that ICME2 was compressing ICME1 from behind. (There are a few times when the perpendicular heat flux is comparable to the parallel one, which raised a concern that some of the data might be contaminated. We decided to show the heat flux data, as there could also be a localized mechanism associated with the CME–CME interaction that breaks down the gyrotropic motion of the particles with respect to the magnetic field.)
The above observations indicate how an almost ‘perfect’ combination of coronal and interplanetary conditions could produce an extreme solar wind disturbance near 1 AU. First, an earlier large CME should occur at the right time to have a minimal deceleration of the later CMEs. It should occur neither too early (otherwise there would be no solar wind rarefaction or magnetic field line stretching upstream of the later ones), nor too late so that it would not slowdown the later ones. Second, the later CMEs should be launched in quick succession. They interact as close to the Sun as possible, so their expansion would be inhibited after the eruptions. The fast transit to 1 AU due to the preconditioning of the upstream solar wind by the earlier CME would significantly reduce the time for them to expand as well. An explicit assumption is that the propagation directions of these CMEs are close to each other. An event with extremely enhanced internal magnetic field and extremely high solar wind speed near 1 AU can be generated under these circumstances besides the initial active region conditions, as we have seen from the 23 July 2012 event.
The present results show how interactions between consecutive CMEs resulted in a ‘perfect storm’ near 1 AU, that is, nonlinear amplification of the events into an extreme one. At least three effects of CME–CME interactions are discovered from the 23 July 2012 event: a change in the propagation direction towards a head-on impact with STEREO A, an extreme enhancement of the ejecta magnetic field and an exceptionally modest deceleration. Combined together, these effects caused a record solar storm near 1 AU since the dawn of the space era. Had the event hit the Earth, it would have produced a record geomagnetic storm with a minimum Dst of −1,150 to −600 nT. This new view on the generation of extreme space weather, especially how a magnetic field larger than 100 nT was produced inside an ICME near 1 AU and preconditioning of the heliosphere for minimal CME deceleration, emphasizes the crucial importance of CME–CME interactions in space weather research and forecasting as previously postulated21,22,40,41,42,43.
These results can serve as a benchmark for space weather prediction models, especially for testing the high-end distributions of the speed and magnetic field of solar wind transients of which detailed observations have been extremely lacking. A preliminary MHD modelling indicates that, while some of the features described here can be captured (that is, rarefaction and field line stretching by preceding eruptions), the solar wind speed and magnetic field near 1 AU are significantly underestimated. Clearly, to create a realistic simulation that can reproduce the key space weather elements, the physical processes associated with the CME–CME interactions have to be taken into account and properly treated. Also note that the 23 July 2012 superstorm occurred in a historically weak solar cycle. Observations of such a solar superstorm during a very weak solar cycle indicate that extreme events are not as infrequent as we imagine. Only with multi-point remote-sensing and in situ observations can we catch the event in its entirety, obtain a complete view of what was happening around the Sun and in the heliosphere and discover for the first time how a combination of coronal and interplanetary conditions produced such an extreme event near 1 AU. These would have far-reaching implications for solar and heliospheric physics as well as space weather research and forecasting.
Estimate of the D st index
where is a correction to Dst, I represents the energy injection to the ring current, τ is the decay time of the ring current, P is the solar wind dynamic pressure, and b and c are constants. The injection I is driven by the solar wind dawn–dusk electric field, vBs, where v is the solar wind speed and Bs is the southward component of the interplanetary magnetic field. Therefore, the solar wind speed and magnetic field are two key elements in the generation of geomagnetic storms. A major difference between the two approaches is that the decay time τ is constant in the formula of Burton et al.33 but varies with vBs in that of O'Brien and McPherron34. This results in different Dst profiles as we see from Fig. 5. Although both of the models have been successful in reproducing observed Dst values, they were largely drawn from geomagnetic storms with Dst >−200 nT. Application of the formulae to extreme storms like the present one should be taken with caution, and one should compare different approaches to get a reliable conclusion.
How to cite this article: Liu, Y. D. et al. Observations of an extreme storm in interplanetary space caused by successive coronal mass ejections. Nat. Commun. 5:3481 doi: 10.1038/ncomms4481 (2014).
The research was supported by the Recruitment Programme of Global Experts of China under grant Y3B0Z2A99S, by the SPORT project under grant XDA04060801, by the Specialized Research Fund for State Key Laboratories of China, by the CAS/SAFEA International Partnership Programme for Creative Research Teams and by the STEREO project under grant NAS5-03131. C.J.F. and A.B.G. acknowledge NASA STEREO grant to UNH. C.M. has received funding from the European Union Seventh Framework Programme (FP7/2007-2013) under grant agreement No. 263252 [COMESEP] and was supported in part by a Marie Curie International Outgoing Fellowship within the 7th European Community Framework Programme. We acknowledge the use of data from STEREO and SOHO, and thank C.T. Russell and D. Odstrcil for helpful discussion.
Two consecutive prominence eruptions and corresponding nascent coronal mass ejections (CMEs) viewed from STEREO B. This movie is made of composite images of EUVI at 304 Å and COR1 from STEREO B with their fields of view to scale. The times are shown in the bottom left corner of the movie.
STEREO B panoramic view of the CME evolution from the Sun to the outer corona. This movie is made of composite images of EUVI at 304 Å, COR1 and COR2 from STEREO B with their fields of view to scale. When the leading edge of the first CME had already reached the field of view of COR2, the second CME and its eruptive prominence were still within the field of view of COR1. Note a transition layer ahead of the CME front, which may indicate a shock signature.
STEREO A panoramic view of the CME evolution from the Sun to the outer corona. This movie is made of composite images of EUVI at 304 Å, COR1 and COR2 from STEREO A with their fields of view to scale. The complex CMEs were obviously directed toward STEREO A. The white dots (known as a 'snowstorm') are produced by energetic particles impacting the cameras.