On the Deceleration of CMEs in the Corona and Interplanetary Medium deduced from Radio and White-Light Observations M. J. Reiner , M. L. Kaisery and J.-L. Bougeret Catholic University and NASA/Goddard Space Flight Center, Greenbelt, MD 20771, USA yNASA/Goddard Space Flight Center, Greenbelt, MD 20771, USA Observatoire de Paris, Meudon, France Abstract. It is generally acknowledged that CMEs, especially the faster ones, must deceleration somewhere between the high corona and interplanetary medium. However, the detailed characteristics and spatial region over which this deceleration occurs is still largely unknown. Simultaneous radio and white-light observations can provide information on the speed profiles of the CME or CME/shock in the high corona and/or interplanetary medium. These observations are consistent with constant deceleration for most CMEs. From the theoretical or modelling point of view, it is usually assumed that the deceleration of CMEs is due to a drag term, which is usually taken to be proportional to the relative speed of the CME compared to that of the solar wind or to this relative speed squared. We point out that such a form for the drag force on the CME inevitably leads to speed profiles that are inconsistent with both the radio and white-light observations. above 2R, the fits to the height-time data are generally consistent with constant deceleration [6]. Modellers, on the other hand, argue that once the CME is released from the sun it is subject to a drag force as it propagates through the interplanetary plasma. The analytical form of this drag force is unknown. However, modellers generally assume that, in analogy with objects falling through the atmosphere, it is proportional to the density and the relative speed squared. In this paper we demonstrate that such a form for the drag force on the CME is not consistent with the observed radio and white-light data. INTRODUCTION It is well known that CME speeds measured in the coronagraph are generally significantly higher than the speeds implied either by their transit times to spacecraft far from the sun or by the in-situ measured shock speeds [19, 18, 5]. However, the spatial regime over which the deceleration occurs and the detailed characterization of the corresponding speed profiles are not well established, due in part to the fact that the coronagraph measurements extend only out to 30R . Many CMEs, generally the faster ones, can drive shocks that, in turn, can generate low-frequency radio emissions [3, 1]. Since the density in the corona and interplanetary medium falls off with increasing heliocentric distance, these type II radio emissions will decrease in frequency as the CME/shock moves farther from the sun. Thus these frequency-drifting radio emissions can provide an alternative method of measuring CME dynamics. Such radio measurements have the advantage that they measure the radial speed or ’true" speed of the shock. Therefore, they can be particularly useful for deducing the dynamics for halo, Earth-directed CMEs, where projection effects are important [7]. Furthermore, the low-frequency radio observations can extend the distance range to well beyond 30R [8, 2, 10]. In those cases where there is significant deceleration implied by the time-sequence of white-light coronagraph images, it is generally found that, at least for most CMEs RADIO AND WHITE-LIGHT OBSERVATIONS OF A CME/SHOCK In order to describe and understand the dynamics of CMEs, it is necessary to make time sequenced, remote observations of signatures of the CME as it propagates through the solar corona and/or interplanetary medium. One way of doing this is to analyze the time sequence of images made by white-light coronagraphs. An alternative way of measuring the dynamics of CMEs is to use the observed frequency drift of the radio emissions generated by the shock driven ahead of the CME [12, 17]. Both these methods are complementary. The white-light observations are more direct but have the difficulty that they are only plane-of-sky observations (which require CP679, Solar Wind Ten: Proceedings of the Tenth International Solar Wind Conference, edited by M. Velli, R. Bruno, and F. Malara © 2003 American Institute of Physics 0-7354-0148-9/03/$20.00 152 Radio observation for the January 14, 2002 CME unknown projection effect corrections) and that they only extend out to 30R . The radio observations, on the other hand, measure the radial motion and can extend all the way to 1 AU and beyond, but are less direct in that the observations are made in the frequency domain and therefore require a density model in order to convert to the spatial regime. The limitations of each of these methods suggest that the best approach therefore is to use the combined radio and white-light data and to determine the CME dynamics by requiring consistency between the simultaneous radio and white-light observations [16]. The frequency-drifting type II emissions generated by this January 14 CME are shown in dynamic spectrum in Figure 2. A GOES M4.4 LDE X-ray, with peak intensity at 06:27 UT, was associated with this radio event. As is usually the case, this CME associated flare was accompanied by a very intense and complex type IIIlike radio burst [11, 14], which is the dominant (overexposed) feature shown in Figure 2. The weaker, much more slowly drifting, diffuse radio emissions in Figure 2, observed from 07 : 30 to 10 : 00 UT, are the type II radio emissions that were generated as the CME/shock propagated through the high corona and interplanetary medium. To more readily discern the relationship between these frequency-drifting radio emissions and the CME dynamics, we have plotted the dynamic spectrum as inverse frequency versus time [9, 10]. The reason for doing this is that in the interplanetary medium the plasma density falls off as 1=R2, where R is the heliocentric distance, so that the observed radio frequency must scale as 1/R. Thus plotting the radio dynamic spectrum as 1/f versus time is essentially equivalent to plotting it as R versus time. The dashed black straight lines in Figure 2 then correspond to the CME/shock moving through the interplanetary medium at a constant speed. We get two straight lines, one with half the slope of the other, corresponding to radio emissions at either the fundamental or harmonic of the plasma frequency (as labelled). We assumed that the diffuse type II emissions were at the harmonic. The solid black curves in Figure 2, which provide a somewhat better fit to the observed frequency drift of the type II emissions, corresponds to the shock moving with a constant deceleration of 14 m s;2 (see below). The height-time and velocity-time relation corresponding to this fit is shown by the solid curves in Figure 1. These curves are clearly consistent with the observed white-light LASCO data for this near-limb CME. White-light observation for the January 14, 2002 CME On January 14, 2002 the SOHO/LASCO coronagraph observed a white-light CME propagating outward from SW solar limb. It first appeared in LASCO C2 at 05:40 UT at a height of 2:7R; it was visible in C3 at least to 09:00 UT, when it was at 26R. We estimated the leading edge height of the CME in each LASCO image and display the corresponding height-time data by the dots in Figure 1a. The CME initially accelerated until about 06:15 UT. However, after 06:15 UT the height-time data can be fit either with a straight line (corresponding to a constant speed of 1463 km/s) or with a modest deceleration (see below). The solar origin of this CME is not known (there were no SOHO/EIT images), however the SOHO/MDI images suggest a possible active site near the western limb. Hence this height-time data may be close to the true height-time relationship for this CME. R (Rs) (a) (b) v(km/s) Speed profile for the January 14, 2002 CME Possible speed profiles for the CME/shock can be determined from the measured parameters of the shock when it was observed in-situ. We then try to select the "true" speed profile by requiring that the corresponding height-time profile simultanouesly fit both the whitelight CME height-time data and the frequency-drifting radio data [15]. The CME-driven shock for this event was observed at Wind at 05:25 UT on January 17, 2002, corresponding to a transit time to Earth of 71 hours, and therefore a transit speed of 587 km s;1 . From the values of the plasma Time (UT) FIGURE 1. (a) Height-time plot for the CME observed on January 14, 2002. (b) Corresponding velocity-time profile (see text) 153 January 14, 2002 1/frequency (kHz) Type II Emissions H Type III Burst F 06:00 07:00 08:00 09:00 10:00 11:00 Time (UT) FIGURE 2. Dynamic spectrum of the Wind/WAVES radio emissions observed from 06:00 to 11:00 UT on January 14, 2002 in the frequency band from 100 kHz to 14 MHz. This is a plot of the intensity of the radio emissions as a function of inverse frequency (vertical axis) and time (horizontal axis). parameters on either side of the shock, assuming a gas hydrodynamic shock, we estimated a shock speed of 403 km s;1 . The fact that this shock speed is significantly lower than the transit speed suggests that the CME/shock must have decelerated between the sun and Earth. Some of this discrepancy could also be due to the fact that at Earth we observed the flank of this western-directed shock. However, we ignore this additional complication here; it is not critical to our argument. Consistent with the low-frequency type II radio data [12], we assume that the CME/shock accelerated at a constant rate, a, until time, ta , i.e., v = vo + at, after which it moved at a constant speed, v1AU , to 1 AU. The determination of the acceleration profile, i.e., a and ta , then depends on the initial speed vo , the measured shock speed v1AU at 1 AU, and the transit time to 1 AU. Since in the present case the transit time to 1 AU and the shock speed at 1 AU are known, for any given initial CME speed, vo , we get a unique solution for the CME speed profile from the sun to 1 AU. Specifically, for the January 14, 2002 event, if we assume an initial CME speed of 1500 km s;1 at 06:15 UT, when the CME/shock was at 5:3R, then the known transit time (71 hours) and the speed of the CME shock at 1 AU (403 km s;1 ) requires an acceleration of a = ;14 m s;2 and a deceleration time of ta = 22 hours. The corresponding speed profile, as a function of time (to 100 R), is shown by the solid curve in Figure 1b and, as a function of heliocentric distance (to 1 AU), by the solid curve in Figure 3a. The height-time relationship calculated from this speed profile is shown by the solid curve in Figure 1a and the acceleration relationship, in Figure 3b. The height-time profile is clearly consistent with the LASCO height-time data measured for this CME. Now, in order to compare this CME speed profile with the frequency-drifting type II emissions in Figure 2, we next need to convert the corresponding height-time relationship in Figure 1a to a frequency-time relationship. To do this we assumed a 1=R2 falloff of the plasma density in the interplanetary medium. Then, we adjusted the value of the density at 1 AU in order that this corresponding frequency versus time curve provide a "best fit" to the type II frequency drift over the entire frequency range of the type II emissions shown in Figure 2. This procedure gave the solid black curves in Figure 2. This fit, which corresponds to the best overall simultaneous fit to the radio and white-light data, corresponded to a density, normalized at 1 AU, of 15 cm;3. This procedure can be repeated for other assumed initial speeds for the CME, in each case solving for the deceleration and deceleration time, given the contraints imposed by the known transit time and the shock speed at 1 AU. In each case, we determined the "best fit" to the frequency drifting type II data by adjusting the density at 1 AU. Each case will yield a somewhat different curve on the 1=f versus time dynamic spectrum. For example, an initial speed of 1800 km/s, would require an acceleration of a = ;23 m s;2 and a deceleration time, ta = 6.25 hours, with density at 1 AU of 24 cm ;3. However, this solution (not shown) does not provide as good a simultaneous fit to the white-light and radio data. CME DECELERATION VIA A DRAG FORCE In the above example we have shown that the speed profile of the CME or CME/shock deduced from the frequency drift of the type II radio emissions and the CME height-time measurements is consistent with con- 154 stant deceleration for a finite time period. On the other hand, modellers typically assume that the deceleration of CMEs in the solar corona and interplanetary medium is caused by a drag force [4]. This drag force, FD , is commonly assumed to be proportional to v 2 , i.e., FD / Av2 , where is the plasma density of the medium (corona or interplanetary medium), A is the effective area, and v is the speed relative to the medium. If this drag force is the primary cause of CME deceleration, then it is clear that this will lead to a CME deceleration that is not constant in time. To illustrate this we suppose that, after the initial ejection of the CME, this drag force and gravity (which gives only a small contribution) are the only forces acting on the CME. Then we have, ent. There is no way that we can adjust the parameters so that the solution would provide a reasonable fit either to the white-light height-time data or to the frequency drift of the type II radio emissions. These results then suggest that the commonly assumed analytical expression for the drag force is inconsistent with the CME dynamics implied by both the observed radio and white-light observations, i.e. it will lead to a CME velocity profile that is inconsistent with the data. Either this is not the correct form for the actual drag force acting on the CME or the drag force is not what causes the CME to decelerate. It is also clear that using a drag term proportional to the velocity will also yield a nonconstant deceleration, which is inconsistent with observations. 2 m ddtR2 = G MR2m ; CD 2o Ao (v ; vsw )2 CONCLUSION (1) where CD is the drag coefficient, m is the CME mass, vsw is the solar wind speed, G is the gravitational constant and M is the solar mass. In writing Eq. (1) we assumed that = o =R2 and that A = Ao R2. Eq. (1) was then solved for the speed profile. We did this by starting with the known shock speed at 1 AU and then integrating Eq. (1) inward towards the sun. The values of the various parameters for this CME are unknown, so we simply started with typical values, which were then adjusted until the solution approached 1R after 71 hours. As typical values we have taken o = 50 10;20 kg m;3, CD = 0:5, m = 1:0 1012 kg, A = 0:6 1021 m2 , vsw = 3:5 105 m s;1 , v = 4:0 105 m s;1 , The solution to Eq. 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