Multiple ground-based and satellite observations of global Pi 2 magnetic pulsations

• Main Authors: Yumoto, K., Takahashi, K., Sakurai, T., Sutcliffe, P. R., Kokubun, S.
• Format: Other/Unknown Material
• Language: unknown
• Published: 1990
• Subjects: 46; EISCAT; Iceland
• Online Access: http://ntrs.nasa.gov/search.jsp?R=19900063383

Four Pi 2 events are examined using data obtained concurrently at the Syowa-Iceland conjugate stations, the EISCAT-Magnetometer Cross, low-latitude stations HER on the nightside and KAK on the dayside, and at AMPTE/CCE in the outer magnetosphere during the period from 2300 UT on May 22 to 0300 UT on May 23, 1985. Several characteristics of Pi 2 are established on the basis of high time resolution magnetic field data. First of all, horizontal components, H and D, of the Pi 2 oscillate nearly antiphase and in-phase, respectively, between the high- and low-altitude stations in the midnight southern hemisphere. Both H and D components of the Pi 2 have nearly in-phase relationships between the nightside and the dayside stations at low altitude. The Pi 2 amplitude is larger at the high-latitude station and decreases toward low latitudes. The dominant periods of the Pi 2 are nearly identical at all stations.