paper

How accurately can we measure the reconnection rate for the MMS diffusion region event of 2017-07-11?

arXiv:1808.03603 · doi:10.1029/2018JA025711

Abstract

We investigate the accuracy with which the reconnection electric field can be determined from in-situ plasma data. We study the magnetotail electron diffusion region observed by NASA's Magnetospheric Multiscale (MMS) on 2017-07-11 at 22:34 UT and focus on the very large errors in that result from errors in an boundary-normal coordinate system. We determine several coordinates for this MMS event using several different methods. We use these axes to estimate . We find some consensus that the reconnection rate was roughly =3.2 mV/m 0.06 mV/m, which corresponds to a normalized reconnection rate of . Minimum variance analysis of the electron velocity (MVA-), MVA of , minimization of Faraday residue, and an adjusted version of the maximum directional derivative of the magnetic field (MDD-) technique all produce {reasonably} similar coordinate axes. We use virtual MMS data from a particle-in-cell simulation of this event to estimate the errors in the coordinate axes and reconnection rate associated with MVA- and MDD-. The and directions are most reliably determined by MVA- when the spacecraft observes a clear electron jet reversal. When the magnetic field data has errors as small as 0.5\% of the background field strength, the direction obtained by MDD- technique may be off by as much as 35. The normal direction is most accurately obtained by MDD-. Overall, we find that these techniques were able to identify from the virtual data within error bars 20\%.

arXiv commentSubmitted to JGR - Space Physics

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