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Achieving zero current for polar wind outflow on open flux tubes subjected to large photoelectron fluxes
Author(s) -
Wilson G. R.,
Khazanov G.,
Horwitz J. L.
Publication year - 1997
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/97gl00923
Subject(s) - ionosphere , magnetosphere , polar wind , physics , flux (metallurgy) , electron , outflow , polar , substorm , geophysics , solar wind , photoelectric effect , atomic physics , computational physics , atmospheric sciences , plasma , meteorology , magnetopause , materials science , nuclear physics , astronomy , optics , metallurgy
In this study we investigate how the condition of zero current on open flux tubes with polar wind outflow, subjected to large photoelectron fluxes, can be achieved. We employ a steady state collisionless semikinetic model to determine the density profiles of O + , H + , thermal electrons and photoelectrons coming from the ionosphere along with H + , ions and electrons coming from the magnetosphere. The model solution attains a potential distribution which both satisfies the condition of charge neutrality and zero current. For the range of parameters considered in this study we find that a 45–60 volt discontinuous potential drop may develop to reflect most of the photoelectrons back toward the ionosphere. This develops because the downward flux of electrons from the magnetosphere to the ionosphere on typical open flux tubes (e.g. the polar rain) appears to be insufficient to balance the photoelectron flux from the ionosphere.