STEADY-STATE MAGNETIC-FIELD CONFIGURATIONS FOR THE EARTHS MAGNETOTAIL

[11] IS STEADY CONVECTION POSSIBLE IN THE EARTHS MAGNETOTAIL [J]. GEOPHYSICAL RESEARCH LETTERS, 1980, 7 (11) : 897 - 900

[12] ERICKSON GM, 1984, GEOPHYS MONOGR SER, V30, P296, DOI DOI 10.1029/GM030P0296

[13] ERICKSON GM, 1985, THESIS RICE U HOUSTO

[14] A TURBULENT MECHANISM FOR SUBSTORM ONSET IN THE EARTHS MAGNETOTAIL [J]. GEOPHYSICAL RESEARCH LETTERS, 1987, 14 (04) : 367 - 370

[15] THE MAGNETIC-FIELD OF THE EQUATORIAL MAGNETOTAIL FROM 10-RE TO 40-RE [J]. JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, 1986, 91 (A4): : 4238 - 4244

[16] FUCHS K, 1979, GEOPHYS MONOGR SER, V21, P86

[17] Galeev A.A., 1976, JETP, V43, P1113

[18] EFFECT OF A LOCALIZED MINIMUM IN EQUATORIAL FIELD-STRENGTH ON RESISTIVE TEARING INSTABILITY IN THE GEOMAGNETOTAIL [J]. JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, 1987, 92 (A5): : 4745 - 4750

[19] Hones E. W., 1984, GEOPHYS MONOGR SER, V30, P178

[20] HONES EW, 1979, SPACE SCI REV, V23, P393, DOI 10.1007/BF00172247

[11] IS STEADY CONVECTION POSSIBLE IN THE EARTHS MAGNETOTAIL [J]. GEOPHYSICAL RESEARCH LETTERS, 1980, 7 (11) : 897 - 900

[12] ERICKSON GM, 1984, GEOPHYS MONOGR SER, V30, P296, DOI DOI 10.1029/GM030P0296

[13] ERICKSON GM, 1985, THESIS RICE U HOUSTO

[14] A TURBULENT MECHANISM FOR SUBSTORM ONSET IN THE EARTHS MAGNETOTAIL [J]. GEOPHYSICAL RESEARCH LETTERS, 1987, 14 (04) : 367 - 370

[15] THE MAGNETIC-FIELD OF THE EQUATORIAL MAGNETOTAIL FROM 10-RE TO 40-RE [J]. JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, 1986, 91 (A4): : 4238 - 4244

[16] FUCHS K, 1979, GEOPHYS MONOGR SER, V21, P86

[17] Galeev A.A., 1976, JETP, V43, P1113

[18] EFFECT OF A LOCALIZED MINIMUM IN EQUATORIAL FIELD-STRENGTH ON RESISTIVE TEARING INSTABILITY IN THE GEOMAGNETOTAIL [J]. JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, 1987, 92 (A5): : 4745 - 4750

[19] Hones E. W., 1984, GEOPHYS MONOGR SER, V30, P178

[20] HONES EW, 1979, SPACE SCI REV, V23, P393, DOI 10.1007/BF00172247