A method is reported to determine, by data of the
ground-based magnetic observations in polar cap, the quasi-sectorial (with
periodicity from 7 to 27 days) SS* structures in the interplanetary magnetic
field (IMF) BY component. The BY effect in the polar cap magnetic variations is
revealed only under summer condition, when the high ionospheric conductivity
ensures availability of ionospheric current systems, responsible for
appropriate magnetic disturbances. It is shown that BY structures,
reconstructed from the polar cap magnetic data during summer months, are in
best conformity with actual variations of the IMF By component, measured
onboard the ACE spacecraft in the Lagrange point L1. The reported method can be
used for identification of the actual IMF BY component coupling with the
magnetosphere. A great advantage of the method over other methods, based on the
satellite measurements, is permanent, on-line available information on the real
solar wind parameters affecting the magnetosphere. It implies that the BY IMF
component, identified by the ground-based magnetic data, can be applied to
verify and to validate information on solar wind parameters
(https://omniweb.gsfc.nasa.gov/), obtained by distant monitors far upstream of
the magnetosphere.
Author(s) Details:
O. A. Troshichev,
Arctic
and Antarctic Research Institute, Russia.
Please see the link here: https://stm.bookpi.org/EIEGES-V6/article/view/13066
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