Complexity Of The 18 October 1995 Magnetic Cloud Observed by Wind and the Multi-Tube Magnetic Cloud Model. V.A. Osherovich1, J. Fainberg2, A. Vinas2 and R. Fitzenreiter2 1 EER Systems Inc., NASA/GSFC, Greenbelt, MD 20771, 2 NASA/GSFC Greenbelt, MD 20771, US Abstract. The notion that a magnetic cloud may consist not of one but of a few closely interacting magnetic tubes came from the analysis of the relation between the electron temperature Te and plasma density Ne (1Fainberg et al. 1996). The log-log plot of Te versus Ne of data in the 10-13 June 1993 Ulysses magnetic cloud revealed two polytropes (both with ge < 1) which have been attributed by 2Osherovich, Fainberg and Stone (1999a) to two helices embedded in the same cylindrical flux rope. In contrast to configurations with cylindrical symmetry, magnetic configurations with helical symmetry allow a description of many helices which in cross section look like distorted flux ropes. We present elements of the magnetic and thermodynamic structure of the Oct 18-21, 1995 magnetic cloud observed by Wind. Our research is complementary to previous studies of this cloud by other authors (3Larson et al. 1997; 4Lepping et al. 1997; 5Janoo et al. 1998). The log-log plots of Te vs Ne suggest that this cloud consists of eight magnetic tubes with polytropic indices below unity and a few non-coherent structures for which the polytropic relation is not valid. The solar wind quasiinvariant (6Osherovich et al., 1999b) for this cloud strongly anti-correlates with the Dst index for the resulting magnetic storm. MAGNETIC STRUCTURE OF THE CLOUD AND SELF-SIMILAR (OFB MODEL) FOR A SINGLE FLUX ROPE B2f = -(R / 2) df dR B2z* = f - B2f The October 18-21, 1995 cloud observed by Wind has all three magnetic cloud elements which according to Burlaga [71981] are: a) a significant enhancement of the total magnetic field B (figure 1, blackr line), b) a smooth rotation of the total magnetic field B (figure 2, red line) and c) a low proton temperature Tp. The front sheath is marked by the shock at 11.111h (hours referenced r to start of October 18). Starting from the shock, B rotates (blue line in figure 2), but the rotation in the z-y plane is not smooth. Only on entering the cloud at 19.1h, can one see the beginning of the smooth rotation during r the period 19.104-48.917h. After this period, the B rotation continues in the back sheath (orange curve in figure 2), but the smoothness typical for inside the cloud is lost. (1) (2) where (z*, f, R) are cylindrical coordinates with z* along the axis of the flux rope. Thus, for a "flat top" df cloud like the Oct 18-21,1995 cloud, ª 0 and dR therefore Bf should be close to 0. In fact, we see a large Bf component (green curve in Figure 1). The self-similar model of Osherovich, Farrugia and Burlaga (OFB 1993) has r r r B = B 0 (h)y -2 (t) ez* + B f (h)y -1 (t) e f (3) r y' r r (4) v = R eR + v 0 (h) ez* y where h = R / y(t) is a self-similar parameter. The evolution function y(t) obeys the equation The magnetic structure of the October 18-21,1995 cannot be described by any force-free magnetic flux rope (neither constant nor non-constant alpha). The general solution for a force-free rope [Lust and Schluter, 1954] can be expressed through a generating function where d 2y dy (5) = Sy-2 - Qy-1 + Ky (-2g +1 ) - n 2 dt dt 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/$20.00 733 where S, Q, K and n are constants; g is a polytropic index. In order for the OFB flux rope to expand, g Figure 1. Total magnetic field components for October 18-21, 1995 magnetic cloud observed by Wind. Figure 4. Three types of structures inside the magnetic cloud. Figure 2. Rotation of Magnetic Field Vector in October 18-21,1995 Magnetic Cloud Observed by Wind. Figure 5. Position of three structures inside the magnetic cloud must be below unity for either v 0 (h) = 0 or v 0 (h) ≠ 0 which we include for purpose of generality. The OFB model does accommodate a flat top B profile for an old cloud, when y(t) is large enough and Bf max is comparable to B z* max (over-grown pinch). Figure 3. Total electron temperature vs. density in the magnetic cloud and the sheath 734 ANTI-CORRLELATION OF Te AND Ne IN THE CLOUD AND THE SHEATH correlation with Dst drop during related magnetic storms. The dependence of Te on Ne in the cloud (red dots in figure 3) show eight extended periods with significant anti-correlation (cc > 0.7) between Te and Ne, for which the polytropic relation g e-1 Te = FN e (6) holds. Between those regions (which we interpret as magnetic tubes) there are non-coherent structures with cc < 0.7. For the whole cloud (including non-coherent structures), F=5.87x105 cgs units and ge = 0.39. For the sheath (orange and blue points in figure 3), F is lower and ge is somewhat higher than in the cloud, but is still less than unity. For the back sheath, for example, ge = 0.75 and F = 2.66x105. Three types of structures (highly coherent, coherent and non-coherent) inside the cloud are illustrated in figure 4. The corresponding correlation coefficients are cc =0.93 (blue color) cc = 0.84 (black) and cc = 0.1 (green). Figure 5 illustrates the position r of the corresponding regions on the z-y plane of B rotation. The magnetic structure of the back sheath includes two regions: (strong field region – gray color in figures 6 and 7 and the weak field region – black color on the same figures). Thus, magnetically and thermodynamically, such regions can be separated from each other. Further division (fine structure) is possible. Figure 6. Rotation of magnetic field in back sheath ANOMALY OF SOLAR WIND QUASIINVARIANT (QI) AND MAGNETIC STORM INDUCED BY THE OCTOBER 18-21, 1995 CLOUD Recently, a new index of solar activity, the solar wind quasi-invariant QI ≡ (B 2 / 8p) /(rv 2 / 2) (7) Figure 7. Structures inside the back sheath of the magnetic cloud. has been suggested (Osherovich, Fainberg and Stone, 1999). QI is based only on parameters measured in the solar wind, namely magnetic field strength B, solar wind speed v and density r. While the yearly median values of QI follow yearly sunspot numbers with cc = 0.98, every magnetic cloud can be viewed as a violation of QI (increase by a factor of 20-100). Figure 7 illustrates this increase and also the strong anti- 735 with cc > 0.7 and a number of non-coherent structures between tubes with cc < 0.7. 2. For the whole cloud (including non-coherent regions), ge = 0.39 and F = 5.87x105. For the back sheath, these values are ge = 0.75 and F = 2.66 x105. Thus, for both the cloud and the sheath ge < 1 but g e is significantly larger in the sheath as was previously observed in the June 10-13, 1993 Ulysses cloud [Fainberg et al. 1996; Osherovich and Burlaga 1997]. 3. The cloud is old (expansion subsided) and as such is in agreement with the OFB model where it has an overgrown Bf component which leads to a flat profile. 4. We interpret the complexity of this cloud (8 tubes) as a case of interacting helices embedded in one cylindrical flux rope (our multi-tube model). Figure 8. Solar wind quasi-invariant increase for the magnetic cloud and the related drop in Dst index. 5. The abnormally large QI for this cloud closely anticorrelates with the Dst index, which dropped during the associated magnetic storm. DISCUSSION AND CONCLUSIONS From the analysis of total Te as a function of Ne, we infer that most of clouds consist of a few magnetic tubes wrapped up in a magnetic flux rope (container). Our exact bounded MHD solutions have depicted such configuration as multiple helices embedded in the cylindrical flux rope (Krat and Osherovich, 1976; Osherovich, Fainberg and Stone, 1999b). The topological complexity of such solutions depends on the magnetic flux function (ground-statersolution, first excited state, etc.). The continuity of B everywhere and finite magnetic energy per unit of length of the main tube, makes such solutions, mathematically, similar to eigen-functions in quantum mechanics (Osherovich, 1975). The complex structure of magnetic clouds like the October 18-21, 1995 cloud, we believe has consequences for the interaction of such clouds with planetary magnetospheres and comets. The strongly non-Maxwellian distribution of electrons in magnetic clouds (discovered by Fainberg et al. 1996) leads to an abnormally high population of highly ionized heavy ions, which in turn can cause soft-x-rays during the collision with comets. This internal complexity could be a source of additional variability of such x-rays. REFERENCES 1. Fainberg, J. et al., Solar Wind 8, 554, 1996. 2. Osherovich, V.A., J. Fainberg and R.G. Stone GRL 26(3), 401, 1999a.. 3. Larson, DE et al., Adv. Space Res. 20 (4-5), 655, 1997. 4. Lepping RP et al., J Geophys Res-Space 102 (A7): 14049, 1997. 5. Janoo, L et al., J Geophys Res-Space 103 (A8): 1724917259, 1998. 6. Osherovich, V.A., J. Fainberg and R.G. Stone GRL 26(16), 2597, 1999b. 7. Burlaga, L.F., E. Sittler, F. Mariani and R. Schwenn, J. Geophys. Res. 86, 6673, 1981. 8. Lust, R. and A. Schluter, Z. Astrophys. 34, 263, 1954. 9. Osherovich, V.A. C. Farrugia and L.F. Burlaga, Adv. Space Res/. 13, 6(6), 57, 1993. 10. Krat, V.A. and V.A. Osherovich, Solar Phys., 59, 43, 1978. CONCLUSIONS 11. Osherovich, V.A., Soln. Dann. 8, 1975. 12. Osherovich, V.A. and L.F. Burlaga, in Coronal Mass Ejections, eds N. Crooker, J. Joselyn and J. Feynman, 157, 1997. 1. The October 18-21, 1995 cloud contains eight magnetic tubes, for which Te anti-correlates with Ne 736
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