Driving dayside convection with northward IMF:: Observations by a sounding rocket launched from Svalbard

被引:20
|
作者
Maynard, NC
Burke, WJ
Pfaff, RF
Weber, EJ
Ober, DM
Weimer, DR
Moen, J
Milan, S
Måseide, K
Sandholt, PE
Egeland, A
Soraas, F
Lepping, R
Bounds, S
Acuña, MH
Freudenreich, H
Machuzak, JS
Gentile, LC
Clemmons, JH
Lester, M
Ning, P
Hardy, DA
Holtet, JA
Stadsnes, J
van Eyken, T
机构
[1] Mission Res Corp, Nashua, NH 03062 USA
[2] USAF, Res Lab, Bedford, MA 01731 USA
[3] NASA, Goddard Space Flight Ctr, Extraterr Phys Lab, Greenbelt, MD 20771 USA
[4] Univ Courses Svalbard, N-9170 Longyearbyen, Norway
[5] Univ Leicester, Dept Phys, Leicester LE1 7RH, Leics, England
[6] Univ Oslo, Dept Phys, N-0316 Oslo, Norway
[7] Univ Bergen, Dept Phys, N-5007 Bergen, Norway
[8] Boston Coll, Inst Sci Res, Chestnut Hill, MA 02467 USA
[9] Aerosp Corp, Los Angeles, CA 90009 USA
[10] Keo Consultants, Brookline, MA 02445 USA
[11] Svalbard European Incoherent Scatter Radar, N-9170 Longyearbyen, Norway
关键词
D O I
10.1029/1999JA900462
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
The first sounding rocket flight into the dayside cusp with dark ground and northward interplanetary magnetic field (IMF) conditions was launched from the new SvalRak range at Ny-Alesund in the Svalbard archipelago in early December 1997. Extensive ground observations of auroral emissions and radar backscatter provided contexts for in situ rocket measurements. Real-time interplanetary measurements from the Wind satellite aided launch selection with foreknowledge of impending conditions. NASA rocket flight 36.153 was launched near local magnetic noon while the IMF was dominated by positive B-X and had lesser northward B-Z and negative B-Y components. The rocket's westward trajectory carried it toward auroral forms associated with morningside boundary layers. The rich set of vector de electric and magnetic fields, energetic particles, thermal plasma, plasma waves, and optical emissions gathered by the rocket reveal a complex electrodynamic picture of the cusp/boundary-layer region. Four factors were important in separating temporal and spatial effects: (1) Near the winter solstice the Earth's north magnetic pole tilts away from the Sun, (2) at the UT of the flight the dipole axis was rotated toward dawn, (3) the variability of solar wind driving was low, and (4) B-X was the dominant IMF component. We conclude that no signatures of dayside merging in the Northern Hemisphere were detected in either the rocket or ground sensors. Electric field variations in the interplanetary medium directly correlate with those observed by the sounding rocket, with significantly shorter lag times than estimated for simple propagation between Wind and the ionosphere. The correlation requires that the observed Northern Hemisphere convection structures were stirred in part by merging of the IMF with closed field lines in the Southern Hemisphere, thereby adding open flux to the northern polar cap. Subsequent motions of adiaroic polar cap boundaries were detected in the rocket electric field measurements. The observations indicate that IMF B-X significantly affected the location and timing of merging interactions.
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收藏
页码:5245 / 5263
页数:19
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