Magnetic reconnection is a fundamental plasma process that governs the interaction and transfer of energy between plasma populations. On the dayside of an intrinsic planetary magnetosphere, magnetic reconnection between the interplanetary magnetic field (IMF) and the planetary field facilitates the transfer of energy between the Sun and the plasma environment of the planet, while changing magnetic topology and accelerating local plasma (e.g., Dungey, 1961;Slavin et al., 2010). The likelihood of reconnection to occur along a dayside magnetopause depends on the orientation of the magnetic fields adjacent to the boundary, among other factors. That is, reconnection is more likely to occur when the two magnetic field regimes are antiparallel, or highly sheared, to one another. For example, Earth possesses a global, intrinsic magnetic dipole field which points northward at the magnetic equator, and therefore exhibits a preference for southward IMF orientation for dayside magnetopause reconnection to occur (e.g., Crooker, 1979;Dungey, 1963). However, given the complexity of the crustal magnetic field environment around Mars, a more extensive analysis is required to determine the preferred conditions for reconnection to take place across the dayside magnetosphere.The magnetosphere of Mars primarily differs from Earth's due to a lack of a global magnetic dynamo field. Instead, Mars possess crustal magnetic anomalies that are scattered across the surface of the planet (Acuña et al., 1999). These crustal fields protrude out into space creating many "minimagnetospheres" that comprise a dynamic and varied magnetic environment for the Mars-solar wind interaction (Brain et al., 2003). Variations in the crustal field location due to diurnal and seasonal changes constantly alter the planetary obstacle to the solar wind. These nonuniform planetary fields, coupled with the dynamics of the system, lead to a much different interaction than what has been observed at intrinsic magnetospheres. In regions where the crustal magnetic fields are weak, the Martian conducting ionosphere acts as the primary obstacle to the solar wind flow, leading to the IMF draping around the planet (e.g., Luhmann et al., 2004;Ma et al., 2002). Despite the lack of a global, intrinsic magnetic field at Mars, observations of magnetic reconnection have been reported throughout