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Ann. Geophys., 30, 1727-1741, 2012
https://doi.org/10.5194/angeo-30-1727-2012
© Author(s) 2012. This work is distributed under
the Creative Commons Attribution 3.0 License.
Regular paper
20 Dec 2012
Remote estimation of reconnection parameters in the Earth's magnetotail: model and observations
A. Alexandrova1,*, R. Nakamura1, V. S. Semenov2, I. V. Kubyshkin2, S. Apatenkov2, E. V. Panov1, D. Korovinskiy1, H. Biernat1, W. Baumjohann1, K.-H. Glassmeier3,4, and J. P. McFadden5 1Space Research Institute, Austrian Academy of Sciences, Graz, Austria
2St. Petersburg State University, St. Petersburg, Russia
3TU Braunschweig, Braunschweig, Germany
4Max-Planck Institute of Solar System Research, Katlenburg-Lindau,Germany
5Space Science Laboratory, University of California, Berkeley, CA, USA
*Invited contribution by A. Alexandrova, recipient of the EGU Outstanding Student Poster (OSP) Award 2011.
Abstract. We develop a method to estimate the reconnected magnetic flux and the location of the reconnection site using properties of magnetic field and plasma velocity disturbances in the regions surrounding the reconnection plasma flow. Our analysis is based on a 3-D non-steady reconnection model with a finite-sized X-line length. In this framework, we obtain a system of equations capturing the relationships between the disturbances of the magnetic field and plasma flow from one side and the reconnection characteristics from another side. These equations allow us to determine the reconnection characteristics from one-point remote observations of the reconnection fast flow, propagated in the magnetotail current sheet. We apply the model to magnetic field and plasma observations at (−43, −11.2, −6.9) RE GSM obtained by the THEMIS/ARTEMIS spacecraft, located in the tail lobe during a substorm event. We found that the reconnection region was located at ~ (−27, 3.5, 0) RE GSM. The X-line appeared to be close to the local time of the substorm current wedge identified from ground-based observations. We estimated the total magnetic flux, which was reconnected in the event as ~5 MWb. That corresponds to a small fraction of the total amount of magnetic flux transferred during a substorm.

Citation: Alexandrova, A., Nakamura, R., Semenov, V. S., Kubyshkin, I. V., Apatenkov, S., Panov, E. V., Korovinskiy, D., Biernat, H., Baumjohann, W., Glassmeier, K.-H., and McFadden, J. P.: Remote estimation of reconnection parameters in the Earth's magnetotail: model and observations, Ann. Geophys., 30, 1727-1741, https://doi.org/10.5194/angeo-30-1727-2012, 2012.
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