Electric current and magnetic field geometry in flapping magnetotail current sheets
Electric current and magnetic field geometry in flapping magnetotail current sheets
复制标题
DOI:
10.5194/angeo-23-1391-2005
复制
发表时间:
2005-06
影响因子:
1.9
通讯作者:
A. Runov;V. Sergeev;Wolfgang Baumjohann;R. Nakamura;S. Apatenkov;Y. Asano;M. Volwerk;Z. Vörös
中科院分区:
文献类型:
--
作者:
A. Runov;V. Sergeev;Wolfgang Baumjohann;R. Nakamura;S. Apatenkov;Y. Asano;M. Volwerk;Z. Vörös
Using four-point magnetic field measurements by the Cluster spacecraft, we statistically analyze the magnetic field and electric current configurations during rapid cross- ings of the current sheet observed in July-October 2001 at geocentric distances of 19 RE. The database includes 78 crossings, specially selected to apply multi-point data analy- sis techniques to calculate vector derivatives. Observed bipo- lar variations of jz, often with |jz|>jy , indicate that the elec- tric currents follow kinks of the current sheet. The current density varies between 5-25 nA/m 2 . The half-thickness of the current sheet during flapping varies over a wide range, from 1 to 20 ion thermal gyroradii (Lcp, calculated from av- erage temperature and lobe magnetic field for each crossing). We found no relationship between the tilt angle of the cur- rent sheet normal and the half-thickness. In 68 cases the magnetic field curvature vector has a positive (earthward) X-component. Ten cases with a negative (tailward) cur- vature, associated with reconnection, were detected within 0<YGSM<7RE. The minimum curvature radii vary mainly between 1 and 10Lcp, and the adiabaticity parameter 1 for 73% of the events. The electric current density during flapping is often off-central, i.e. the main current density is shifted from the neutral sheet (|Bx|<5 nT) to the Northern or Southern Hemisphere. This is most likely a temporal ef- fect related to the flapping. The analysis shows that the flap- ping motion of the current sheet is associated with kink-like waves on the sheet surface. The kink fronts, tilted in the Y Z plane, moved toward dawn in the morning half and to- ward dusk in the evening half of the magnetotail.