Auroral morphology of the midday oval

Auroral displays in the noon sector were examined by using hundreds of Defense Meteorological Satellite Program auroral images, taken over the southern polar region in austral winters, in order to determine the morphology. The auroral displays in the midday part of the auroral oval can be grouped into five characteristic types, depending on the geomagnetic activity and the Bz component of the interplanetary magnetic field. An important characteristic is the clear disconnection in appearance between the noonside and the nightside discrete auroras. Also, there is the lack of correlation between the concurrent nightside substorm activity and midday discrete auroral activity. Thus, the occurrence of bright, discrete auroras in the midday oval may be caused by the local injection of the magnetosheath plasma into the dayside boundary layer. The observed discontinuity of discrete auroras between the dayside and the nightside ovals is consistent with the existence of two separated major injection regions along the auroral oval: the dayside cusp and the nightside plasma sheet.

[1]  J. Whitteker,et al.  The topside magnetospheric cleft ionosphere observed from the Isis 2 spacecraft , 1976 .

[2]  S. Mende,et al.  Systematics in auroral energy spectra , 1972 .

[3]  S. Akasofu,et al.  Auroral oval photographs from the DMSP 8531 and 10533 satellites , 1976 .

[4]  C. Anger,et al.  The instantaneous relationship between polar cap and oval auroras at times of northward interplanetary magnetic field , 1982 .

[5]  C. Anger,et al.  Topside optical view of the dayside cleft aurora , 1976 .

[6]  S.-I. Akasofu,et al.  Dayside and nightside auroral arc systems , 1980 .

[7]  C. Meng Polar cap arcs and the plasma sheet , 1981 .

[8]  R. Hoffman,et al.  Observational evidence for a boundary layer source of dayside region 1 field‐aligned currents , 1981 .

[9]  C. P. Pike,et al.  The midday, discrete auroral gap , 1978 .

[10]  B. Sonnerup Theory of the low-latitude boundary layer , 1980 .

[11]  E. Dubinin,et al.  Solar wind energy transfer regions inside the dayside magnetopause: Accelerated heavy ions as tracers for MHD-processes in the dayside boundary layer , 1985 .

[12]  J. Winningham,et al.  Auroral emissions and particle precipitation in the noon sector , 1972 .

[13]  Christopher T. Russell,et al.  ISEE observations of flux transfer events at the dayside magnetopause , 1979 .

[14]  G. Sivjee,et al.  Particle and optical measurements in the magnetic noon sector of the auroral oval , 1975 .

[15]  C. Meng Electron precipitation in the midday auroral oval , 1981 .

[16]  C. D. Anger,et al.  Characteristics of dayside 5577Å and 3914Å aurora , 1977 .

[17]  V. Vasyliūnas Interaction between the magnetospheric boundary layers and the ionosphere , 1979 .

[18]  R. Lundin Solar wind energy transfer regions inside the dayside magnetopause. II: Evidence for an MHD generator process , 1984 .

[19]  T. Potemra,et al.  Field‐aligned currents in the dayside cusp observed by Triad , 1976 .

[20]  G. Paschmann,et al.  The frontside boundary layer of the magnetosphere and the problem of reconnection , 1977 .

[21]  L. Frank Plasma in the Earth's polar magnetosphere , 1971 .

[22]  J. Winningham,et al.  Penetration of magnetosheath plasma to low altitudes through the dayside magnetospheric cusps , 1971 .

[23]  C. Meng,et al.  Electron precipitation equatorward of the auroral oval and the mantle aurora in the midday sector , 1983 .

[24]  S. Akasofu,et al.  The continuity of the auroral oval in the afternoon sector , 1975 .

[25]  C. Meng,et al.  Dynamics of the aurora—IV: Polar magnetic substorms and westward traveling surges , 1966 .

[26]  E. W. Hones,et al.  Structure of the low‐latitude boundary layer , 1980 .

[27]  M. Saunders,et al.  Interpretation of magnetic field perturbations in the earth's magnetopause boundary layers , 1983 .

[28]  D. Evans The Characteristics of a Persistent Auroral Arc at High Latitude in the 1400 MLT Sector , 1985 .

[29]  B. Dandekar Relationship between the IMF, the midday gap, and auroral substorm activity , 1979 .

[30]  C. Anger,et al.  Characteristics of the instantaneous auroral oval in the 1200–1800 MLT sector , 1981 .

[31]  S. Akasofu Recent progress in studies of DMSP auroral photographs , 1976 .

[32]  E. W. Hones,et al.  The magnetospheric boundary layer: Site of plasma, momentum and energy transfer from the magnetosheath into the magnetosphere , 1976 .

[33]  Syun-Ichi Akasofu,et al.  The development of the auroral substorm. , 1964 .

[34]  R. Lundin,et al.  Boundary layer plasmas as a source for high-latitude, early afternoon, auroral arcs , 1985 .

[35]  G. Shepherd,et al.  Magnetospheric Dayside Cusp: A Topside View of Its 6300-Angstrom Atomic Oxygen Emission , 1973, Science.

[36]  E. Dubinin,et al.  Solar wind energy transfer regions inside the dayside magnetopause. I: Evidence for magnetosheath plasma penetration , 1984 .