Interplanetary magnetic field properties and variability near Mercury's orbit. Issue 8 (24th August 2017)

• Record Type: Journal Article
• Authors: James, Matthew K.; Imber, Suzanne M.; Bunce, Emma J.; Yeoman, Timothy K.; Lockwood, Mike; Owens, Mathew J.; Slavin, James A.
• Is Part Of: Journal of geophysical research. Volume 122:Issue 8(2017)
• Page Start: 7907
• Page End: 7924
• Publication Date: 2017-08-24
• Subjects: MESSENGER -- Mercury -- solar wind -- IMF; Magnetospheric physics -- Periodicals; Space environment -- Periodicals; Cosmic physics -- Periodicals; Planets -- Atmospheres -- Periodicals; Heliosphere (Astrophysics) -- Periodicals; Geophysics -- Periodicals; 523.01
• DOI: 10.1002/2017JA024435
• Languages: English
• ISSNs: 2169-9380

Abstract

Abstract: The first extensive study of interplanetary magnetic field (IMF) characteristics and stability at Mercury is undertaken using MErcury Surface, Space ENvironment, GEochemistry, and Ranging (MESSENGER) magnetometer data. Variations in IMF and solar wind conditions have a direct and rapid effect upon Mercury's highly dynamic magnetosphere; hence, understanding of the time scales over which these variations occur is crucial because they determine the duration of magnetospheric states. We characterize typical distributions of IMF field strength, clock angle, and cone angle throughout the duration of MESSENGER's mission. Clock and cone angle distributions collected during the first Earth year of the mission indicate that there was a significant north‐south asymmetry in the location of the heliospheric current sheet during this period. The stability of IMF magnitude, clock angle, cone angle, and IMF B z polarity is quantified for the entire mission. Changes in IMF B z polarity and magnitude are found to be less likely for higher initial field magnitudes. Stability in IMF conditions is also found to be higher at aphelion (heliocentric distance r ∼ 0.31 AU) than at perihelion ( r ∼ 0.47 AU). Key Points: The typical characteristics of the IMF at Mercury during the MESSENGER mission have been studied The time scales over which variations in the IMF at Mercury occur have been quantified IMF clock and cone angle distributions show long‐term variations related to an asymmetric reversal of the solar dipole