Field line draping about fast coronal mass ejecta: A source of strong out‐of‐the‐ecliptic interplanetary magnetic fields

Fast coronal mass ejecta interact strongly with the ambient interplanetary plasma and magnetic field into which they propagate. A shock forms in front of an ejection and the slower moving ambient plasma ahead is accelerated and deflected from its path. In this paper we argue that such flow accelerations and deflections of the ambient plasma must produce a draping of the ambient interplanetary magnetic field about the ejected material similar to that which occurs in the magnetosheath surrounding the earth's magnetosphere. The draping pattern should depend upon the overall size and shape of the ejection, its speed relative to the ambient plasma ahead, the orientation of the ambient magnetic field, and the position where the shocked plasma is sampled. At some locations upstream from an ejection draping leads to an enhancement of the out-of-the-ecliptic field component (BZ) at the expense of the ecliptic components (BX, BY). Although turbulence and fluctuations in the ambient field may confuse the observational situation, we suggest that draping probably plays an important role in producing intervals of strong and prolonged negative BZ in the ecliptic plane at 1 AU and thus also may be an important factor in stimulating geomagnetic activity.

[1]  L. Burlaga,et al.  Interplanetary magnetic clouds at 1 AU , 1982 .

[2]  Russell A. Howard,et al.  Coronal mass ejections - 1979-1981 , 1985 .

[3]  J. Gosling Large‐scale inhomogeneities in the solar wind of solar origin , 1975 .

[4]  C. Russell,et al.  An empirical relationship between interplanetary conditions and Dst , 1975 .

[5]  A. Hundhausen Interplanetary shock waves and the structure of solar wind disturbances , 1972 .

[6]  C. Fälthammar,et al.  Relationship between changes in the interplanetary magnetic field and variations in the magnetic field at the Earth's surface , 1967 .

[7]  H. Rosenbauer,et al.  Coronal mass ejections and interplanetary shocks , 1985 .

[8]  C. Russell,et al.  Magnetic configuration of the Venus magnetosheath , 1986 .

[9]  J. Slavin,et al.  Giacobini‐Zinner magnetotail: ICE magnetic field observations , 1986 .

[10]  A. Hundhausen,et al.  Solar cycle modulation of galactic cosmic rays: Speculation on the role of coronal transients , 1981 .

[11]  L. Burlaga,et al.  Intense interplanetary magnetic fields observed by geocentric spacecraft during 1963–1975 , 1979 .

[12]  C. Russell,et al.  The magnetotail and substorms , 1973 .

[13]  E. W. Hones,et al.  Field‐aligned plasma flow in MHD simulations of magnetotail reconnection and the formation of boundary layers , 1986 .

[14]  W. Bostick Experimental Study of Ionized Matter Projected across a Magnetic Field , 1956 .

[15]  E. W. Hones Magnetotail: its generation and dissipation , 1976 .

[16]  D. Baker,et al.  Bidirectional solar wind electron heat flux events , 1987 .

[17]  R. L. Arnoldy,et al.  SIGNATURE IN THE INTERPLANETARY MEDIUM FOR SUBSTORMS. , 1971 .

[18]  D. L. Webster,et al.  Magnetic and electric fields in the magnetosheath , 1970 .

[19]  E. W. Hones,et al.  Substorm associated traveling compression regions in the distant tail: Isee‐3 Geotail observations , 1984 .

[20]  D. Fairfield The ordered magnetic field of the magnetosheath , 1967 .

[21]  C. Russell,et al.  Mapping the magnetosheath field between the magnetopause and the bow shock: Implications for magnetospheric particle leakage , 1984 .

[22]  T. Rosenberg,et al.  Relationship of interplanetary parameters and occurrence of magnetospheric substorms , 1971 .

[23]  S. Smerd,et al.  80 MHz Radioheliograph Evidence on Moving Type IV Bursts and Coronal Magnetic Fields , 1971 .

[24]  P. McIntosh,et al.  Disappearing solar filaments: A useful predictor of geomagnetic activity , 1981 .

[25]  Syun-Ichi Akasofu,et al.  Energy coupling between the solar wind and the magnetosphere , 1981 .

[26]  C. Russell,et al.  Magnetic field draping against the dayside magnetopause , 1985 .