![Hier klicken, um den Treffer aus der Auswahl zu entfernen](images/unchecked.gif) |
Titel |
Evaluation of the generalized Ohm’s law at the subsolar magnetopause diffusion region with MMS data. |
VerfasserIn |
Giulia Cozzani, Alessandro Retino, Olivier Le Contel, Francesco Califano, Alexandros Chasapis, Yuri Khotyaintsev, Laurent Mirioni, Andris Vaivads, Benoit Lavraud, Hugo Breuillard |
Konferenz |
EGU General Assembly 2017
|
Medientyp |
Artikel
|
Sprache |
en
|
Digitales Dokument |
PDF |
Erschienen |
In: GRA - Volume 19 (2017) |
Datensatznummer |
250138348
|
Publikation (Nr.) |
EGU/EGU2017-1330.pdf |
|
|
|
Zusammenfassung |
Magnetic reconnection is a fundamental process occurring in thin current sheets where a
change in the magnetic field topology leads to fast magnetic energy conversion into energy
of charged particles. A key yet poorly understood aspect is how the reconnection electric
field is sustained in the diffusion region by the different terms in the generalized Ohm’s law.
In particular, the role of the pressure and inertia terms is not yet fully understood as well as
the importance of the anomalous resistivity term and its source. Simulations have provided
some estimations of the different terms; however direct observations have been scarce so
far. The four-spacecraft Magnetospheric Multiscale Mission (NASA/MMS) allows, for the first
time, the full evaluation of the generalized Ohm’s law in the diffusion region. Here we present
MMS observations at a few subsolar diffusion region crossings on October,3 rd 2015 where
MMS spacecraft were separated by ~ 25 km. We compare the measured electric field with
the electric field due to both kinetic effects (electron pressure tensor, electron inertia terms)
and to anomalous resistivity associated to different wave modes. The electric field is
balanced by the Hall term at ion scales as expected. At smaller scales, preliminary results
indicate that the electric field is mainly balanced by the divergence of the electron pressure
tensor, although the contribution of anomalous resistivity is not negligible. |
|
|
|
|
|