THEORETICAL STUDY OF THE BURSTY BULK FLOWS IN EARTH’S PLASMA SHEET
Received date: 2000-11-09
Revised date: 2001-01-05
Online published: 2001-08-01
The short duration, fast moving events in the Earth’s plasma sheet have received quite a lot of attentions recently. Such events were termed bursty bulk flows after the paper by Angelopoulos et al. These flow pulses usually last for 10 minutes and have flow speed above 400 km/s. The present paper gives a brief review of the study on the bursty bulk flows. Current theory suggested that the bursty bulk flows are the flows of bubble (underpopulated magnetic flux tube) in the plasma sheet. Under the action of interchange instability, bubble is propelled earthward. Birkeland currents flow at the boundary between the bubble and the background medium, downward the ionosphere from the dawn side boundary and upward from the dusk side boundary. The cross section of a bubble at the equatorial plane would have an elongated streamline shape with the cross tail size of the order of 2 Earth radius. Bubble picture naturally explains characteristics of the bursty bulk flows observed in the plasma sheet. Some numerical simulations have reproduced the observed high-speed flow and the shape of the line of associated magnetic field. Observations have confirmed the expected bubble property, which includes its cross tail size, speed, more dipolar magnetic field, decrease in pressure and density, ionospheric and ground signatures. Both theoretic calculation and observation have demonstrated that the bursty bulk flows are the main mechanism for the magnetic flux and plasma particles transport in the Earth's plasma sheet.
Key words: Bursty bulk flows; Magnetic flux tube; Plasma sheet
CHEN Chuxin . THEORETICAL STUDY OF THE BURSTY BULK FLOWS IN EARTH’S PLASMA SHEET[J]. Advances in Earth Science, 2001 , 16(4) : 584 -586 . DOI: 10.11867/j.issn.1001-8166.2001.04.0584
[1] Angelopoulos V, Baumjohann W, Kennel C F, et al. Bursty bulk flows in the inner central plasma sheet[J]. J Geophys Res, 1992, 97: 4 027-4 039.
[2] Baumjohann W, Paschmann G, Lühr H. Characteristics of high-speed ion flows in the plasma sheet[J]. J Geophys Res, 1990, 95: 3 801-3 809.
[3] Sergeev V A, Angelopoulos V, Gosling J T, et al. Detection of localized, plasma-depleted flux tubes or bubbles in the midtail plasma sheet[J]. J Geophys Res, 1996, 101: 10 817-10 826.
[4] Kauristie K, Sergeev V A, Kubyshkina M, et al. Ionospheric current signatures of transient plasma sheet flows[J]. J Geophys Res, 2000, 105: 10 677-10 690.
[5] Wolf R A. The quasi-static (slow-flow) region of the magnetosphere[A]. In: Carovillano R L, Forbes J M, eds. Solar Terrestrial Physics: Principles and Theoretical Foundations[C]. Hingham: D. Reidel, 1983. 303-368.
[6] Erickson G M, Wolf R A. Is steady convection possible in the Earth's magnetotail?[J]. Geophys Res Lett, 1980, 7: 897-900.
[7] Pontius D H Jr, Wolf R A. Transient flux tubes in the terrestrial magnetosphere[J]. Geophys Res Lett, 1990, 17: 49-52.
[8] Chen C X, Wolf R A. Interpretation of high-speed flows in the plasma sheet[J]. J Geophys Res, 1993, 98: 21 409-21 419.
[9] Chen C X, Wolf R A. Theory of thin-filament motion in Earth's magnetotail and its application to bursty bulk flows[J]. J Geophys Res, 1999, 104: 14 613-14 626.
[10] Angelopoulos V, Phan T D, Larson D E, et al. Magnetotail flow bursts: association to global magnetospheric circulation, relationship to ionospheric activity and direct evidence for localization[J]. Geophys Res Lett, 1997, 24: 2 271-2 274.
[11] Henderson M G, Reeves G D, Murphree J S. Are north-south aligned auroral structures an ionospheric manifestation of bursty bulk flows?[J]. Geophys Res Lett, 1998, 25: 3 737-3 740.
[12] Lyons L R, Nagai T, Blanchard G T, et al. Association between Geotail plasma flows and auroral poleward boundary intensifications observed by CANOPUS photometers[J]. J Geophys Res, 1999, 104: 4 485-4 500.
[13] Sergeev V A, Sauvaud J -A, Popescu D, et al. Multiple-spacecraft observation of a narrow transient plasma jet in the Earth's plasma sheet[J]. Geophys Res Lett, 2000, 27: 851-854.
[14] Amm O, Pajunpä äA, Brandström U. Spatial distribution of conductances and currents associated with a north-south auroral form during a multiplesubstorm period[J]. Ann Geophys, 1999, 17: 1 385-1 396.
[15] Yeoman T K, Lühr H. CUTLASS/IMAGE observations of highlatitude convection features during substorms[J]. Ann Geophys, 1997, 15: 692-702.
[16] Slavin J A, Fairfield D H, Lepping R P, et al. WIND, GEOTAIL, and GOES 9 observations of magnetic field dipolarization and bursty bulk flows in the near-tail[J]. Geophys Res Lett, 1997, 24: 971-974.
[17] Fairfield D H, Mukai T, Lui A T Y, et al. Geotail observations of substrm onset in the inner magnetotail[J]. J Geophys Res, 1998, 103: 103-117.
[18] Shiokawa K, Baumjohann W, Haerendel G, et al. High-speed ion flow, substorm current wedge, and multiple Pi 2 pulsations[J]. J Geophys Res, 1998, 103: 4 491-4 507.
[19] Sergeev V A, Angelopoulos V, Mitchell D G, et al. In situ observations of magnetotail reconnection prior to the onset of a small substorm[J]. J Geophys Res, 1995, 100: 19 121-19 133.
[20] Petrukovich A A, Sergeev V A, Zelenyi L M, et al. Two spacecraft observations of a reconnection pulse during an auroral breakup[J]. J Geophys Res, 1998, 103: 47-59.
/
| 〈 |
|
〉 |