A Statistical Investigation of Factors Influencing the Magnetotail Twist at Mars

The Martian magnetotail exhibits a highly twisted configuration, shifting in response to changes in polarity of the interplanetary magnetic field's (IMF) dawn-dusk (B-Y) component. Here, we analyze similar to 6000 MAVEN orbits to quantify the degree of magnetotail twisting (theta(Twist)) and assess variations as a function of (a) strong planetary crustal field location, (b) Mars season, and (c) downtail distance. The results demonstrate that theta(Twist) is larger for a duskward (+B-Y) IMF orientation a majority of the time. This preference is likely due to the local orientation of crustal magnetic fields across the surface of Mars, where a +B-Y IMF orientation presents ideal conditions for magnetic reconnection to occur. Additionally, we observe an increase in theta(Twist) with downtail distance, similar to Earth's magnetotail. These findings suggest that coupling between the IMF and moderate-to-weak crustal field regions may play a major role in determining the magnetospheric structure at Mars.