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Thermal Variability in the Martian Upper Atmosphere within the Crustal Magnetic Field Region Induced by Gravity Wave Dissipation Due to Ion-drag EffectASTRONOMICAL JOURNALIF5.12025-02-030OA
A linearized coupled model of acoustic-gravity waves and the lower ionosphere at MarsASTRONOMY & ASTROPHYSICSIF5.82024-08-011OA
The siphonic energy transfer between hot solar wind and cold martian ionosphere through open magnetic flux ropeFUNDAMENTAL RESEARCHIF6.32024-07-012OAAI
Gas physisorption impact on prolate dust in free-molecule flows: A static studyPHYSICS OF FLUIDSIF4.32024-05-150PRE
Ion Loss within a Reconnection Exhaust near Mars: MAVEN ObservationsASTROPHYSICAL JOURNALIF5.42023-09-142OA
Density-dependent drag coefficient for gas-adsorbed particles in free-molecule flowsPHYSICS OF FLUIDSIF4.32023-05-191PRE
Electron density variability in the day-side ionosphere of Mars: The role of gravity wavesMONTHLY NOTICES OF THE ROYAL ASTRONOMICAL SOCIETYIF4.82022-11-225PRE
Direct simulation Monte Carlo of the gas-adsorption of particles in gas-particle flowsPHYSICS OF FLUIDSIF4.32022-08-024PRE
The Solar Wind Parker Spiral Angle Distributions and Variations at 1 auASTROPHYSICAL JOURNALIF5.42022-05-314OA