Comparison of Solar Wind Interaction with Mars and Earth: Energy Transfer

• Published in: The Astrophysical journal Vol. 968; no. 2; pp. 84 - 91
• Main Authors: Zhang, H. X., Lu, J. Y., Wang, M., Zhou, Y.
• Format: Journal Article
• Language: English
• Published: Philadelphia The American Astronomical Society 01-06-2024; IOP Publishing
• Subjects: Dipoles; Earth; Energy; Energy transfer; Interplanetary magnetic field; Interplanetary magnetic fields; Magnetic fields; Magnetohydrodynamics; Magnetopause; Magnetopause reconnection; Mars; Numerical simulations; Planetary magnetic fields; Planetary magnetospheres; Solar energy; Solar wind; Southern Hemisphere
• ISSN: 0004-637X; 1538-4357
• DOI: 10.3847/1538-4357/ad463c

Using a global magnetohydrodynamics numerical simulation, this work compares the interaction of the solar wind with Mars and Earth from the perspective of energy transfer under north–south interplanetary magnetic fields (IMFs). Mars lacks a global dipole magnetic field like Earth’s and instead has a small-scale crustal magnetic field near highlands in the southern hemisphere. Unlike Earth’s magnetopause reconnection (at the subsolar point or tail under a southward IMF, or behind the cusp under a northward IMF), the reconnection of the Martian magnetic pileup boundary (MPB) occurs near solar zenith angle (SZA) ≈ 45° (SZA ≈ 30° and 60°) for a southward (northward) IMF, resulting in asymmetric energy transfer between the northern and southern hemispheres. The Martian outflow of mechanical energy appears near SZA ≈ 45° (SZA ≈ 30° and 60°) under a southward (northward) IMF, accompanied by an inflow due to the process of “solar wind pickup.” For energy transfer across the MPB, whether the IMF is northward or southward, the input of electromagnetic energy is twice as large as the input of mechanical energy, which is similar to Earth’s magnetopause for a southward IMF, but opposite to it for a northward IMF. The energy transfer rate of the MPB is slightly higher in a northward IMF than in a southward one, whereas the energy transfer rate of Earth’s magnetopause is far higher in a southward IMF than in a northward one.